{"id":142481,"date":"1993-01-01T00:00:00","date_gmt":"1993-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-mineralogica-y-geoquimica-del-transito-mioceno-plioceno-en-las-cuencas-de-vera-y-sorbas-almeria\/"},"modified":"1993-01-01T00:00:00","modified_gmt":"1993-01-01T00:00:00","slug":"caracterizacion-mineralogica-y-geoquimica-del-transito-mioceno-plioceno-en-las-cuencas-de-vera-y-sorbas-almeria","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/caracterizacion-mineralogica-y-geoquimica-del-transito-mioceno-plioceno-en-las-cuencas-de-vera-y-sorbas-almeria\/","title":{"rendered":"Caracterizacion mineralogica y geoquimica del transito mioceno-plioceno en las cuencas de vera y sorbas (almeria)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Angel Sanchez Bellon <\/strong><\/h2>\n<p>Se ha realizado el estudio de materiales del transito mioplioceno en las cuencas de vera y sorbas, el cual ha tenido diferentes interpretaciones por diferentes autores. Con este estudio se colabora a la solucion de la polemica establecida aportando informacion obtenida a partir de la mineralogia, cristalografia y geoquimica multielemental e isotopica.  estas disciplinas aportan datos muy interesantes para llegar a determinar los materiales constituyentes de las areas fuente, las condiciones paleoambientales del medio de deposito de las diferentes secuencias estudiadas, asi como el grado de diagenesis que los sedimentos han sufrido a lo largo de su historia. Se llega a la principal conclusion de que peque\u00f1as variaciones del nivel del mar provocan la compartimentacion de las cuencas y la formacion de medios confinados con diferente grado de sedimentacion salina o no salina y con mayor o menor grado de influencia de aguas continentales.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracterizacion mineralogica y geoquimica del transito mioceno-plioceno en las cuencas de vera y sorbas (almeria).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracterizacion mineralogica y geoquimica del transito mioceno-plioceno en las cuencas de vera y sorbas (almeria). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Angel Sanchez Bellon <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/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> Sebastian Pardo Eduardo M.<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Manuel Rodr\u00edguez Gallego <\/li>\n<li>Christine Mosser (vocal)<\/li>\n<li>Antonio Caballero Lopez-lendinez (vocal)<\/li>\n<li>Alberto L\u00f3pez Galindo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Angel Sanchez Bellon Se ha realizado el estudio de materiales del transito mioplioceno en las cuencas de [&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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