{"id":18305,"date":"2002-11-07T00:00:00","date_gmt":"2002-11-07T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/los-complejos-tectonicos-alpujarride-y-malaguide-en-el-sector-oriental-de-la-zona-interna-betica-estratigrafa%c2%ada-relaciones-tectonicas-y-evolucion-paleogeografica-durante-el-triasico\/"},"modified":"2002-11-07T00:00:00","modified_gmt":"2002-11-07T00:00:00","slug":"los-complejos-tectonicos-alpujarride-y-malaguide-en-el-sector-oriental-de-la-zona-interna-betica-estratigrafa%c2%ada-relaciones-tectonicas-y-evolucion-paleogeografica-durante-el-triasico","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/los-complejos-tectonicos-alpujarride-y-malaguide-en-el-sector-oriental-de-la-zona-interna-betica-estratigrafa%c2%ada-relaciones-tectonicas-y-evolucion-paleogeografica-durante-el-triasico\/","title":{"rendered":"Los complejos tect\u00f3nicos alpuj\u00e1rride y mal\u00e1guide en el sector oriental de la zona interna b\u00e9tica. estratigraf\u00eda, relaciones tect\u00f3nicas y evoluci\u00f3n paleogeogr\u00e1fica durante el tri\u00e1sico"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Garc\u00eda Tortosa Francisco Juan <\/strong><\/h2>\n<p>En la presente memoria se muestran los resultados derivados de las investigaciones geol\u00f3gicas llevadas a cabo en cinco sectores del extremo oriental de la zona interna b\u00e9tica, investigaciones que se han centrado en el reconocimiento de las diferentes unidades tect\u00f3nicas alpuj\u00e1rrides y mal\u00e1guides, las relaciones tect\u00f3nicas entre ellas y su estudio estratigr\u00e1fico. El sector principal de los cinco estudiados es el comprendido entre mazarr\u00f3n y cabo de palos. estos sectores presentan una estructura interna fruto de la acutaci\u00f3n de una tect\u00f3nica polif\u00e1sica, de la que caben destacar varias fases compresivas con sentido de translaci\u00f3n tect\u00f3nica hacia el norte; varias fases extensionales posteriores a las anteriores que borran en parte las estructuras previas; y varias fases de fallas de desgarre dextorsas (e-o) y sinistrorsas (ne-so), junto con otras fracturas posteriores de menor importancia.  se han diferenciado una serie de unidades litoestratigr\u00e1ficas de las que cabe destacar un grupo detr\u00edtico, con una formaci\u00f3n de edad paleozoica y otra de edad tri\u00e1sica, y un grupo carbonatado, constituido por varias formaciones mesozoicas y terciarias, habi\u00e9ndose estudiado las de edad tri\u00e1sica.  el an\u00e1lisis estratigr\u00e1fico y estructural ha permitido elaborar un ensayo de evoluci\u00f3n paleogeogr\u00e1fica para tri\u00e1sico de los sectores estudiados, pudi\u00e9ndose destacar que se originaron determinadas franjas paleogeogr\u00e1ficas con caracter\u00edsticas deposicionales similares, que se corresponder\u00edan en parte con los dominios nevado-fil\u00e1bride, alpuj\u00e1rride y mal\u00e1guide. Entre estos dos \u00faltimos dominios exist\u00edan zonas transicionales, representas en parte por las unidades intermedias entre los complejos alpuj\u00e1rride y mal\u00e1guide.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Los complejos tect\u00f3nicos alpuj\u00e1rride y mal\u00e1guide en el sector oriental de la zona interna b\u00e9tica. estratigraf\u00eda, relaciones tect\u00f3nicas y evoluci\u00f3n paleogeogr\u00e1fica durante el tri\u00e1sico<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Los complejos tect\u00f3nicos alpuj\u00e1rride y mal\u00e1guide en el sector oriental de la zona interna b\u00e9tica. estratigraf\u00eda, relaciones tect\u00f3nicas y evoluci\u00f3n paleogeogr\u00e1fica durante el tri\u00e1sico <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Garc\u00eda Tortosa Francisco Juan <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 11\/07\/2002<\/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> Sanz De Galdeano Equiza  Carlos<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Antonio Estevez  rubio <\/li>\n<li>alessandro Iannace (vocal)<\/li>\n<li>michel Durand delga (vocal)<\/li>\n<li>Fernando Simancas cabrera (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Garc\u00eda Tortosa Francisco Juan En la presente memoria se muestran los resultados derivados de las investigaciones geol\u00f3gicas [&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":[27,245,953,3435],"tags":[56862,19204,49387,56861,35712,18978],"class_list":["post-18305","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-estratigrafia","category-geologia","category-geologia-estructural","tag-alessandro-iannace","tag-antonio-estevez-rubio","tag-fernando-simancas-cabrera","tag-garcia-tortosa-francisco-juan","tag-michel-durand-delga","tag-sanz-de-galdeano-equiza-carlos"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/18305","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=18305"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/18305\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=18305"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=18305"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=18305"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}