{"id":45321,"date":"2019-04-30T16:38:13","date_gmt":"2019-04-30T16:38:13","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/mineralogia-de-los-materiales-plioceno-pleistocenos-de-la-depresion-de-guadix-baza-granada\/"},"modified":"2019-04-30T16:38:13","modified_gmt":"2019-04-30T16:38:13","slug":"mineralogia-de-los-materiales-plioceno-pleistocenos-de-la-depresion-de-guadix-baza-granada","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/mineralogia-de-los-materiales-plioceno-pleistocenos-de-la-depresion-de-guadix-baza-granada\/","title":{"rendered":"Mineralogia de los materiales plioceno-pleistocenos de la depresion de guadix-baza (granada)."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Sebastian Pardo Eduardo Manuel <\/strong><\/h2>\n<p>Se analiza la mineralogia de los sedimentos de edad plioceno-pleistocenos de la cuenca guadix-baza. Especial enfasis se pone en el estudio de los filosilicatos  su analisis cuantitativo  su distribucion  asi como estudio de diferentes parametros cristalograficos de estos minerales. Estos datos han permitido diferenciar en esta cuenca varios sectores con ambiente de depositos distintos: lacustres fluviales y marinos asi mismo han permitido determinar queel area fuente primordial se situa al sur de la depresion y esta constituida esencialmente por las rocas del complejo alpujarride.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Mineralogia de los materiales plioceno-pleistocenos de la depresion de guadix-baza (granada).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Mineralogia de los materiales plioceno-pleistocenos de la depresion de guadix-baza (granada). <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Sebastian Pardo Eduardo Manuel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1979<\/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>Manuel Rodr\u00edguez Gallego<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Manuel Rodr\u00edguez Gallego <\/li>\n<li>Juan  Antonio Vera Torres (vocal)<\/li>\n<li>Jos\u00e9 Martin Pozas (vocal)<\/li>\n<li>Rafael Delgado Rodriguez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Sebastian Pardo Eduardo Manuel Se analiza la mineralogia de los sedimentos de edad plioceno-pleistocenos de la cuenca [&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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