{"id":6048,"date":"1995-01-01T00:00:00","date_gmt":"1995-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1995\/01\/01\/mineralogia-y-sedimentologia-del-neogeno-del-sector-centro-occidental-de-la-cuenca-del-tajo\/"},"modified":"1995-01-01T00:00:00","modified_gmt":"1995-01-01T00:00:00","slug":"mineralogia-y-sedimentologia-del-neogeno-del-sector-centro-occidental-de-la-cuenca-del-tajo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/mineralogia-y-sedimentologia-del-neogeno-del-sector-centro-occidental-de-la-cuenca-del-tajo\/","title":{"rendered":"Mineralogia y sedimentolog\u00eda del neogeno del sector centro-occidental de la cuenca del tajo"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Dominguez Diaz M. Carmen <\/strong><\/h2>\n<p>Se realizo un estudio de seis sondeos situados en el sector centro-occidental de la cuenca del tajo. Despues de hacer su descripcion litologica, se efectuo un muestreo de las distintas partes, con el fin de determinar la mineralogia total y caracterizar con mayor precision la mineralogia de arcillas.  las principales tecnicas utilizadas han sido difraccion de rx, microscopia electronica de barrido y transmision y espectrometria de emision atomica por plasma de acoplamiento inductivo.  los resultados han permitido distinguir y caracterizar mineralogicamente las distintas unidades estratigraficas (u. De arcosas, u. De calizas y marcas blancas, u. De arcillas verdes y u. De yesos). Se establecen tres etapas en la evolucion de la cuenca: en la 1 la asociacion mineralogica es yeso-anhidrita-glanberita-halita y magnesita, con illita como mineral de la arcilla mayoritario. En la 2 etapa la paragenesis es dolomita y silicatos de mg (saponita y sepiolita). La 3 etapa corresponde al deposito de la u.  de arcosas y los minerales de la arcilla mayoritarios son beidellitas ferricas y montmorillonitas con menor proporcion de illita.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Mineralogia y sedimentolog\u00eda del neogeno del sector centro-occidental de la cuenca del tajo<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Mineralogia y sedimentolog\u00eda del neogeno del sector centro-occidental de la cuenca del tajo <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Dominguez Diaz M. Carmen <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1995<\/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> Brell Parlade Jos\u00e9 Manuel<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Lorenzo Vilas Minondo <\/li>\n<li>Emilio Galan Huertos (vocal)<\/li>\n<li> Hoyos Guerrero Miguel Angel (vocal)<\/li>\n<li>Francisco Lopez  Aguayo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Dominguez Diaz M. Carmen Se realizo un estudio de seis sondeos situados en el sector centro-occidental 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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,245,953,232],"tags":[5042,23082,22341,1680,14708,5043],"class_list":["post-6048","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-estratigrafia","category-geologia","category-mineralogia","tag-brell-parlade-jose-manuel","tag-dominguez-diaz-m-carmen","tag-emilio-galan-huertos","tag-francisco-lopez-aguayo","tag-hoyos-guerrero-miguel-angel","tag-lorenzo-vilas-minondo"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/6048","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=6048"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/6048\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=6048"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=6048"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=6048"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}