{"id":142630,"date":"1993-01-01T00:00:00","date_gmt":"1993-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-estructura-cortical-del-area-de-union-de-las-cordilleras-iberica-y-beticas-interpretacion-geotectonica-basada-en-datos-gravimetricos\/"},"modified":"1993-01-01T00:00:00","modified_gmt":"1993-01-01T00:00:00","slug":"la-estructura-cortical-del-area-de-union-de-las-cordilleras-iberica-y-beticas-interpretacion-geotectonica-basada-en-datos-gravimetricos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-estructura-cortical-del-area-de-union-de-las-cordilleras-iberica-y-beticas-interpretacion-geotectonica-basada-en-datos-gravimetricos\/","title":{"rendered":"La estructura cortical del area de union de las cordilleras iberica y beticas. interpretacion geotectonica basada en datos gravimetricos."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Santiago Casta\u00f1o Fernandez <\/strong><\/h2>\n<p>Se ha realizado un levantamiento gravimetrico de un area de 11000 km2 en el se espa\u00f1ol y se han interpretado los datos realizando una modelizacion de la corteza terrestre en esta zona.Los resultados permiten concretar la existencia de una corteza entre 28 y 24 km de potencia, que presenta un adelgazamiento en direccion ne y que separa, a nivel cortical, las cordilleras iberica y beticas. La corteza esta tambien engrosada en relacion con el eje betico-balear. Mas superficialmente se observa la existencia de grandes estructuras de importancia regional, como son el corredor de cofrentes-hellin y el accidente de jumilla.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La estructura cortical del area de union de las cordilleras iberica y beticas. interpretacion geotectonica basada en datos gravimetricos.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La estructura cortical del area de union de las cordilleras iberica y beticas. interpretacion geotectonica basada en datos gravimetricos. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Santiago Casta\u00f1o Fernandez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1993<\/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>Andr\u00e9s Carb\u00f3 Gorosabel<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Ramon Capote Del Villar <\/li>\n<li>Albert Casas Ponsati (vocal)<\/li>\n<li>Alfonso Maldonado Zamora (vocal)<\/li>\n<li>Lorenzo Vilas Minondo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Santiago Casta\u00f1o Fernandez Se ha realizado un levantamiento gravimetrico de un area de 11000 km2 en el [&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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