{"id":10642,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1996\/01\/01\/estudio-cristalquimico-de-minerales-metamorficos-en-rocas-basicas-del-complejo-nevado-filabride-cordilleras-beticas\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"estudio-cristalquimico-de-minerales-metamorficos-en-rocas-basicas-del-complejo-nevado-filabride-cordilleras-beticas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-cristalquimico-de-minerales-metamorficos-en-rocas-basicas-del-complejo-nevado-filabride-cordilleras-beticas\/","title":{"rendered":"Estudio cristalquimico de minerales metamorficos en rocas basicas del complejo nevado-filabride (cordilleras beticas)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Fernando Camara Artigas <\/strong><\/h2>\n<p>Contiene tres partes: a) introduccion del contexto geologico y descripcion petrologica incluyendo las condiciones termobarometricas; b) cristalquimica de los piroxenos de las rocas estudiadas con especial enfasis en la influencia del contenido en fe3+ sobre los proceso de orden-desorden; y c) cristalquimica de los anfiboles. Las tecnicas empleadas han sido todas las habituales en petrolog\u00eda para la determinacion del quimismo de la roca y de los minerales junto con difractometria de cristal unico y microscopia electronica de transmision (incluyendo microanalisis) para los aspectos cristalquimicos. Las conclusiones fundamentales se refieren a: condiciones termobarometricas de formacion de las rocas, procedimientos de normalizacion de formulas de piroxenos y anfiboles, la fuerte influencia del contenido en egirina de los piroxenos sobre sus caracteristicas cristalquimicas, y el cierre del hueco de miscibilidad entre anfiboles sodicos y sodo-calcicos a alta temperatura.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio cristalquimico de minerales metamorficos en rocas basicas del complejo nevado-filabride (cordilleras beticas).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio cristalquimico de minerales metamorficos en rocas basicas del complejo nevado-filabride (cordilleras beticas). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Fernando Camara Artigas <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Bruno Messiga (vocal)<\/li>\n<li>Antonio Caballero Lopez-lendinez (vocal)<\/li>\n<li>Roberta Oberti (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Fernando Camara Artigas Contiene tres partes: a) introduccion del contexto geologico y descripcion petrologica incluyendo las condiciones [&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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