{"id":46860,"date":"2020-01-15T22:27:34","date_gmt":"2020-01-15T22:27:34","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-mineralogico-y-metalogenico-de-las-mineralizaciones-de-la-sierra-de-guadarrama-sistema-central-espanol\/"},"modified":"2020-01-15T22:27:34","modified_gmt":"2020-01-15T22:27:34","slug":"estudio-mineralogico-y-metalogenico-de-las-mineralizaciones-de-la-sierra-de-guadarrama-sistema-central-espanol","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-mineralogico-y-metalogenico-de-las-mineralizaciones-de-la-sierra-de-guadarrama-sistema-central-espanol\/","title":{"rendered":"Estudio mineralogico y metalogenico de las mineralizaciones de la sierra de guadarrama (sistema central espa\u00f1ol)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Elena Vindel Catena <\/strong><\/h2>\n<p>En este trabajo se han estudiado las mineralizaciones de la sierra de guadarrama desde el punto de vista mineralogico y metalogenico. Se ha establecido una clasificacion de las mineralizaciones filonianas en base a su paragenesis  estableciendose siete paragenesis tipo algunas de ellas divididas en dos subgrupos. Estas mineralizaciones filonianas presentan una distribucion zonal normal  excentrica y controlada por un gradiente termico  cuyo centro generador se situa cercano al pluton de la cabrera. Se distinguen tres zonas: una interna con mineralizaciones de w  sn  as  una intermedia con mineralizaciones de cu y otra externa con mineralizaciones de pb  zn  ba  f. Ademas en este trabajo se ha estudiado la mineralizacion de tipo estratiforme de otero de herreros (segovia) y se exponen algunas interpretaciones geneticas para explicar su origen.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio mineralogico y metalogenico de las mineralizaciones de la sierra de guadarrama (sistema central espa\u00f1ol)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio mineralogico y metalogenico de las mineralizaciones de la sierra de guadarrama (sistema central espa\u00f1ol) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Elena Vindel Catena <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1980<\/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> Amoros Portoles Jos\u00e9 Luis<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Amoros Portoles Jos\u00e9 Luis <\/li>\n<li> Fuster Casas Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<li>Eduardo Alastrue (vocal)<\/li>\n<li>Antonio Arribas Moreno (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Elena Vindel Catena En este trabajo se han estudiado las mineralizaciones de la sierra de guadarrama desde [&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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