{"id":74250,"date":"2005-01-06T00:00:00","date_gmt":"2005-01-06T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructura-y-evolucion-tectonica-reciente-del-campo-de-dala%c2%adas-y-de-na%c2%adjar-en-el-contexto-del-la%c2%admite-meridional-de-las-cordilleras-beticas-orientales\/"},"modified":"2005-01-06T00:00:00","modified_gmt":"2005-01-06T00:00:00","slug":"estructura-y-evolucion-tectonica-reciente-del-campo-de-dala%c2%adas-y-de-na%c2%adjar-en-el-contexto-del-la%c2%admite-meridional-de-las-cordilleras-beticas-orientales","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estructura-y-evolucion-tectonica-reciente-del-campo-de-dala%c2%adas-y-de-na%c2%adjar-en-el-contexto-del-la%c2%admite-meridional-de-las-cordilleras-beticas-orientales\/","title":{"rendered":"Estructura y evoluci\u00f3n tect\u00f3nica reciente del campo de dal\u00edas y de n\u00edjar en el contexto del l\u00edmite meridional de las cordilleras b\u00e9ticas orientales"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Carlos Mar\u00edn Lechado <\/strong><\/h2>\n<p>El campos de dal\u00edas y el campo de n\u00edjar son dos depresiones pertenecientes al borde norte de la cuenca del mar de albor\u00e1n que en la actualidad est\u00e1 emergido y corresponden a los afloramiento m\u00e1s meridionales de sedimentos ne\u00f3genos y cuaternarios de las zonas internas de las cordilleras b\u00e9ticas orientales.     el estudio de la estructura superficial y profunda y de las deformaciones del relleno ne\u00f3geno y cuaternario y del basamento perteneciente al complejo alpuj\u00e1rride a partir del an\u00e1lisis combinado de datos geol\u00f3gicos de campo y geof\u00edsicos (s\u00edsmica de reflexi\u00f3n, prospecci\u00f3n gravim\u00e9trica y prospecci\u00f3n magn\u00e9tica) ha permitido establecer un modelo de evoluci\u00f3n tect\u00f3nica de la regi\u00f3n desde el tortoniense hasta la actualidad que permite conocer mejor las caracter\u00edsticas del l\u00edmite entre las cordilleras b\u00e9ticas y el mar de albor\u00e1n.     la estructura profunda del campo de dal\u00edas est\u00e1 determinada principalmente por pliegues de crecimiento de orientaci\u00f3n ene-oso desarrollados desde el tortoniense superior hasta el cuaternario y fallas cuaternarias de orientaci\u00f3n no-se y reducido salto. El basamento del campo de n\u00edjar muestra elevaciones y depresiones relacionas con fallas de direcci\u00f3n no-se. La falla de carboneras tiene caracter\u00edsticas diferentes a lo largo de su extensi\u00f3n. En el sector si se acumula el m\u00e1ximo espesor de sedimentos, mientras que en el sector ne se desarrollan pliegues transpresivos como flanco vertical. Las rocas volc\u00e1nica se encuentran ampliamente distribuidas bajo el relleno ne\u00f3geno y cuaternario. La plataforma continental situada al sur del campo de dal\u00edas de n\u00edjar est\u00e1 deformada por pliegues de crecimiento de orientaci\u00f3n ene-oso desde el meridiano de motril hasta el golfo de almer\u00eda y fallas normales de orientaci\u00f3n no-se que afectan a sedimentos pliocuaternarios.     la evoluci\u00f3n tect\u00f3nica de sierra de g\u00e1dor situada al norte del campo de dal\u00edas y formada por rocas del complejo alpuj\u00e1rride, se inicia c<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estructura y evoluci\u00f3n tect\u00f3nica reciente del campo de dal\u00edas y de n\u00edjar en el contexto del l\u00edmite meridional de las cordilleras b\u00e9ticas orientales<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estructura y evoluci\u00f3n tect\u00f3nica reciente del campo de dal\u00edas y de n\u00edjar en el contexto del l\u00edmite meridional de las cordilleras b\u00e9ticas orientales <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Carlos Mar\u00edn Lechado <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/06\/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>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>eulalia Masana closa (vocal)<\/li>\n<li>ahmed Chalouan (vocal)<\/li>\n<li>\u00e1ngel Mart\u00edn-serrano Garc\u00eda (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Carlos Mar\u00edn Lechado El campos de dal\u00edas y el campo de n\u00edjar son dos depresiones pertenecientes al [&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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