{"id":4658,"date":"2018-03-09T00:06:56","date_gmt":"2018-03-09T00:06:56","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/2018\/03\/09\/tectonica-reciente-en-el-margen-iberico-suroccidental\/"},"modified":"2018-03-09T00:06:56","modified_gmt":"2018-03-09T00:06:56","slug":"tectonica-reciente-en-el-margen-iberico-suroccidental","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/tectonica-reciente-en-el-margen-iberico-suroccidental\/","title":{"rendered":"Tectonica reciente en el margen iberico suroccidental"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Enrique Jes\u00fas Flores Hurtado <\/strong><\/h2>\n<p>Se estudia la actividad neotectonica plio-cuaternaria en el extremo occidental de andalucia. Esta tectonica se desenvuelve dentro del acercamiento continuado entre la subplaca iberica (placa euroasiatica) y la placa africana. Es esencialmente fragil y afecta a niveles estructurales muy someros. El maximo eje compresivo seria horizontal y de direccion no-se. Por su parte el eje principal intermedio seria vertical mientras que el eje menor, de direccion ne-sw, seria distensivo. El regimen tectonico general seria una transpresion dextra, que desarrollaria una ancha banda de deformacion, con fracturas tensionales no-se, fallas normales nno-sse, pliegues y fallas oso-ene, y desgarres senestros nno-sse. Durante el cuaternario mas reciente se producen basculamientos ligados a un regimen extensional local, con actuacion de fallas normales de direccion ne-so.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Tectonica reciente en el margen iberico suroccidental<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Tectonica reciente en el margen iberico suroccidental <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Enrique Jes\u00fas Flores Hurtado <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Huelva<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 22\/03\/1994<\/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>Joaquin Rodriguez Vidal<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Goy goy Jos\u00e9 Luis <\/li>\n<li> Sanz de galdeano equiza  Carlos (vocal)<\/li>\n<li>caridad Zazo carde\u00f1a (vocal)<\/li>\n<li>fern\u00e1ndo D\u00edaz del olmo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Enrique Jes\u00fas Flores Hurtado Se estudia la actividad neotectonica plio-cuaternaria en el extremo occidental de andalucia. Esta [&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":[27,953,75,18975],"tags":[18979,18976,18980,7597,18977,18978],"class_list":["post-4658","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geomorfologia","category-huelva","tag-caridad-zazo-cardena","tag-enrique-jesus-flores-hurtado","tag-fernando-diaz-del-olmo","tag-goy-goy-jose-luis","tag-joaquin-rodriguez-vidal","tag-sanz-de-galdeano-equiza-carlos"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/4658","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=4658"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/4658\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=4658"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=4658"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=4658"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}