{"id":72367,"date":"2018-03-09T23:17:10","date_gmt":"2018-03-09T23:17:10","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructura-y-evolucion-tectonica-del-golfo-de-cadirz\/"},"modified":"2018-03-09T23:17:10","modified_gmt":"2018-03-09T23:17:10","slug":"estructura-y-evolucion-tectonica-del-golfo-de-cadirz","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estructura-y-evolucion-tectonica-del-golfo-de-cadirz\/","title":{"rendered":"Estructura y evoluci\u00f3n tect\u00f3nica del golfo de c\u00e1dirz"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Teresa Medialdea Cela <\/strong><\/h2>\n<p>El golfo de c\u00e1diz constituye un \u00e1rea de gran inter\u00e9s tanto por su contexto geodin\u00e1mico , como por la relevancia que adquieren los distintos procesos geol\u00f3gicos que han tenido lugar a lo largo de su compleja evoluci\u00f3n.Esta tesis doctoral pretende contribuir al conocimiento geol\u00f3gico del golfo de c\u00e1diz y su evoluci\u00f3n desde una pespectiva regional, mediante el estudio de las estructuras  tect\u00f3nicas del golfo de c\u00e1diz y de la corteza del margen sudportugu\u00e9s.Con este fin, se han interpretado numerosos perfiles de s\u00ednmica de reflexi\u00f3n multicanal y de refracci\u00f3n\/reflexi\u00f3n de gran \u00e1ngulo.La informaci\u00f3n proporcionada por estos m\u00e9todos de prospecci\u00f3n geof\u00edsica ha sido complementada con otros datos adquiridos con distintas t\u00e9cnicas (sonda multihaz, sparker, dragas, etc)que se han combinado con el fin de correlacionear las estructuras profundas y superficiales y adquirir as\u00ed una imagen m\u00e1s completa de la corteza.  el \u00e1rea de estudio comprende el sector septentrional y central del golfo de c\u00e1diz (talud continental medio e inferior)hasta la zona oriental de la llanura abisal de la herradura y el extremo nororiental de la llanura abisal del sena.A lo largo de esta amplia zoan, se ha caracterizado en primer lugar el basamento  y las unidades sismoestratigr\u00e1ficas que constituyen la cobertera sediemnteria del amargen, para  a continuaci\u00f3n describir las principales estructuras tect\u00f3nicas reconocidas y la unidad al\u00f3ctona del golfo de c\u00e1diz (estructura interna, procesos de deformaci\u00f3n y mecanismos de emplazamiento).El car\u00e1cter singular del talud medio del margen subportugu\u00e9s, en el que se localizan los \u00fanicos afloramientos dela basamento varisco en el margen continental, ha requerido un estudio espec\u00edfico que incluye la descripci\u00f3n de sus principales rasgos y la determianci\u00f3n de la estructura profunda de la corteza y su comparaci\u00f3n con otras zonas del golfo de c\u00e1diz de una serie de dominios tect\u00f3nicos desde el punto de<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estructura y evoluci\u00f3n tect\u00f3nica del golfo de c\u00e1dirz<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estructura y evoluci\u00f3n tect\u00f3nica del golfo de c\u00e1dirz <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Teresa Medialdea Cela <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 20\/01\/2005<\/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>Ram\u00f3n Vegas Mart\u00ednez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: andr\u00e9s Carb\u00f3 gorosabel <\/li>\n<li> Diaz del rio espa\u00f1ol victor (vocal)<\/li>\n<li>Luis Somoza losada (vocal)<\/li>\n<li>Andr\u00e9s Maldonado l\u00f3pez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Teresa Medialdea Cela El golfo de c\u00e1diz constituye un \u00e1rea de gran inter\u00e9s tanto por su contexto [&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 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