{"id":133927,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/emplazamiento-intracortical-y-desmembramiento-extensional-de-los-cuerpos-peridotiticos-de-ronda-y-del-rif-arco-de-gibraltar\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"emplazamiento-intracortical-y-desmembramiento-extensional-de-los-cuerpos-peridotiticos-de-ronda-y-del-rif-arco-de-gibraltar","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/emplazamiento-intracortical-y-desmembramiento-extensional-de-los-cuerpos-peridotiticos-de-ronda-y-del-rif-arco-de-gibraltar\/","title":{"rendered":"Emplazamiento intracortical y desmembramiento extensional de los cuerpos peridotiticos de ronda y del rif (arco de gibraltar)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Mario Sanchez Gomez <\/strong><\/h2>\n<p>La tesis analiza y define los eventos tectonometamorficos que afectan al complejo alpujarride occidental, y se ubica temporal y espacialmente el emplazamiento intracortical de las peridotitas dentro de dicho complejo a traves del registro tanto estructural como metamorfico de las rocas de composicion cortical adyacentes, con una mineralogia y comportamiento mecanico mucho mas favorables para preservar los eventos tectonometamorficos. Los principales resultados y conclusiones que pueden extraerse de este trabajo se detallan a continuacion.  &#8211; sobre conocimiento geologico regional:  realizacion de los mapas geologicos a escala 1:25000 de las areas del cerro del castor, montemayor, guadaiza y ojen (al oeste de malaga), y ceuta y el cabo de tres forcas (rif).  redefinicion de la columna litoestratigrafica de la unidad de ojen atendiendo a criterios petrologicos.  tipificacion de la sucesion litologica de las unidades de grupo de blanca.  caracterizacion de las escamas de montemayor y de los granitoides diatexiticos, granitoides porfidicos y leucogranitos generados en un evento evolutivo tardio.  &#8211; sobre la estructura de las unidades alpujarrides:  analisis de las estructuras desarrolladas sobre la unidad de jubrique en relacion con el ascenso de las peridotitas de ronda (manto litosferico).  cronolog\u00eda relativa de las deformaciones que afectan a la unidad de ojen.  descubrimiento de la intercalacion de las laminas peridotiticas entre otras de naturaleza cortical en los macizos ultramaficos de sierra bermeja y sierra alpujata.  estructuras intrusivas de granitoides tardios entre las laminas peridotiticas y a traves de ellas.  &#8211; sobre el emplazamiento (intracortical) de las peridotitas de ronda:  emplazamiento en contraccion de las escamas ultramaficas de montemayor. Posicion estructural de este haz principal de cabalgamientos.  proceso de desmembracion extensional de las escamas ultramaficas en cuerpos discretos de gra<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Emplazamiento intracortical y desmembramiento extensional de los cuerpos peridotiticos de ronda y del rif (arco de gibraltar).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Emplazamiento intracortical y desmembramiento extensional de los cuerpos peridotiticos de ronda y del rif (arco de gibraltar). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Mario Sanchez Gomez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/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>Victor Garcia Due\u00f1as<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Andres Perez Estaun <\/li>\n<li>Fernando Simancas Cabrera (vocal)<\/li>\n<li> Navidad Fernandez De La Cruz Marina (vocal)<\/li>\n<li>Fernando Gervilla Linares (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Mario Sanchez Gomez La tesis analiza y define los eventos tectonometamorficos que afectan al complejo alpujarride occidental, [&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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