{"id":88291,"date":"2018-03-10T00:13:17","date_gmt":"2018-03-10T00:13:17","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/alteracion-experimental-de-rocas-pertenecientes-a-la-cordillera-betica-y-genesis-de-minerales-de-la-arcilla\/"},"modified":"2018-03-10T00:13:17","modified_gmt":"2018-03-10T00:13:17","slug":"alteracion-experimental-de-rocas-pertenecientes-a-la-cordillera-betica-y-genesis-de-minerales-de-la-arcilla","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/alteracion-experimental-de-rocas-pertenecientes-a-la-cordillera-betica-y-genesis-de-minerales-de-la-arcilla\/","title":{"rendered":"Alteracion experimental de rocas pertenecientes a la cordillera betica y genesis de minerales de la arcilla."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Ahmed Drief <\/strong><\/h2>\n<p>En esta tesis doctoral se estudia la alteraci\u00f3n de diversos tipos de rocas (serpentinitas, micasquistos, filitas, gneises, ofitas) de las cordilleras b\u00e9ticas por molienda y por interacci\u00f3n aj temperatura ambiente con diversas soluciones acuosas (soluci\u00f3n b\u00e1sica naoh 1 m, agua marina, agua marina enriquecida en k). Tambi\u00e9n se estudia el quismo de los minerales de la arcilla formados por los procesos de alteraci\u00f3n baja condiciones naturales (esmectitas en este caso) y expermientales (sustancias amorfas, esmectita, bertheierina, ferro-lizardita). El uso de la difracci\u00f3n de rayos x y de la microscop\u00eda electr\u00f3nica de transmisi\u00f3n anal\u00edtica ha sido generalizado a lo largo de todo el trabajo de esta tesis doctoral, como herramienta imprescindible en la carcterizaci\u00f3n de las diferentes fases minerales formadas dada la baja cristalinidad de las mismas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Alteracion experimental de rocas pertenecientes a la cordillera betica y genesis de minerales de la arcilla.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Alteracion experimental de rocas pertenecientes a la cordillera betica y genesis de minerales de la arcilla. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Ahmed Drief <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 22\/12\/2000<\/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>Fernando Nieto Garcia<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: manuel Rodr\u00edguez gallego <\/li>\n<li>Jos\u00e9 lu\u00eds P\u00e9rez rodr\u00edguez (vocal)<\/li>\n<li>francisca Martinez ruiz (vocal)<\/li>\n<li>Juan Oleves ba\u00f1os (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Ahmed Drief En esta tesis doctoral se estudia la alteraci\u00f3n de diversos tipos de rocas (serpentinitas, micasquistos, [&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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