{"id":25198,"date":"2003-05-09T00:00:00","date_gmt":"2003-05-09T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructuras-tectonicas-recientes-en-la-transversal-central-de-las-cordilleras-beticas\/"},"modified":"2003-05-09T00:00:00","modified_gmt":"2003-05-09T00:00:00","slug":"estructuras-tectonicas-recientes-en-la-transversal-central-de-las-cordilleras-beticas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructuras-tectonicas-recientes-en-la-transversal-central-de-las-cordilleras-beticas\/","title":{"rendered":"Estructuras tect\u00f3nicas recientes en la transversal central de las cordilleras b\u00e9ticas"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Patricia Ruano Roca <\/strong><\/h2>\n<p>Las estructuras tect\u00f3nicas activas en las cordilleras b\u00e9tico-rife\u00f1as acomodan la convergencia oblicua, con orientaci\u00f3n no-se, entre las placas euroasi\u00e1tica y africana. La transversal central de las cordilleras b\u00e9ticas permite entender las relaciones entre las estructuras que deforman las zonas interntas y las zonas externas. A pesar del car\u00e1cter convergente del l\u00edmite de placas, la mayor\u00eda de fallas presentes en esta transversal son normales y muestran un contexto extensional. Sin embargo, la mayor parte de la regi\u00f3n muestra un r\u00e1pido levantamiento desde el mioceno que seria m\u00e1s t\u00edpico de una regi\u00f3n en compresi\u00f3n.  los datos geof\u00edsicos permiten determinar los principales rasgos de la estructura profunda de la regi\u00f3n. Mientras que en el mar de albor\u00e1n los datos de s\u00edsmica de refracci\u00f3n indican la presencia de una corteza continental delgada (15-km), hacia las cordilleras b\u00e9ticas se produce un r\u00e1pido engrosamiento de la corteza de hasta 36-37 km. Los estudios gravim\u00e9tricos indican que el engrosamiento cortical es brusco y se produce en una posici\u00f3n pr\u00f3xima a la l\u00ednea de costa. Los perfieles de s\u00edsmica de reflexi\u00f3n profunda en las cordilleras muestran reflectores horizontales en la corteza inferior que no est\u00e1n afectados por los grandes pliegues de la corteza superior.  la continuidad de anomal\u00edas aeromagn\u00e9ticas del macizo ib\u00e9rico bajo las zonas externas de las cordilleras b\u00e9ticas hacia que dichos materiales constituyen el basamento de estas \u00faltimas. Todos estos datos sugieren que las rocas que forman las cordilleras b\u00e9ticas est\u00e1n despegadas sobre un z\u00f3calo que estar\u00eda constituido por el macizo ib\u00e9rico. Este despegue constituir\u00e1 la principal estructura activa de las cordilleras b\u00e9tica, con un movimiento relativo del bloque de techo hacia el no.  las estructuras observadas en campo a lo largo de la transversal indican que a partir del mioceno superior se han desarrollado, tano pliegues como fallas qu<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estructuras tect\u00f3nicas recientes en la transversal central de las cordilleras b\u00e9ticas<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estructuras tect\u00f3nicas recientes en la transversal central de las cordilleras b\u00e9ticas <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Patricia Ruano Roca <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 05\/09\/2003<\/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>Jes\u00fas Galindo Zaldivar<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Francisco Gonz\u00e1lez lodeiro <\/li>\n<li>Jos\u00e9 Manuel Gonz\u00e1lez casado (vocal)<\/li>\n<li> Sim\u00f3n g\u00f3mez Jos\u00e9 Luis (vocal)<\/li>\n<li>Carlos Sanz de galdeano (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Patricia Ruano Roca Las estructuras tect\u00f3nicas activas en las cordilleras b\u00e9tico-rife\u00f1as acomodan la convergencia oblicua, con orientaci\u00f3n [&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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