{"id":34303,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-de-la-circulacion-hidrotermal-en-granitos-mineralizados-con-w-sn-sierra-de-guadarrama\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"analisis-de-la-circulacion-hidrotermal-en-granitos-mineralizados-con-w-sn-sierra-de-guadarrama","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/analisis-de-la-circulacion-hidrotermal-en-granitos-mineralizados-con-w-sn-sierra-de-guadarrama\/","title":{"rendered":"Analisis de la circulacion hidrotermal en granitos mineralizados con w-sn (sierra de guadarrama)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Eugenia Garcia Garcia <\/strong><\/h2>\n<p>En este trabajo se estudia la forma en que los fluidos hidrotermales asociados a mineralizaciones intragran\u00edticas de w-sn en la sierra de guadarrama han migrado a trav\u00e9s del macizo gran\u00edtico. Se han reconocido tres tipos principales de fluidos: 1) fluidos acuosos hipersalinos del tipo lw-s (inclusiones con halita y otros s\u00f3lidos atrapados) 2) fluidos acuoso-carb\u00f3nicos; (i) inclusiones vc-m-w del sistema h2o-naci- co2-ch4 (ii) inclusiones vc-w del sistema h2o-naci-co2-(ch4) y (iii) fluidos con h2o-naci-(co2)-ch4 del tipo lw-c y 3) fluidos acuosos del tipo lw1 y lw2 diferenciadas por su salinidad y temperatura.  los resultados obtenidos del estudio de la microfracturaci\u00f3n han permitido comprobar como existen cambios significativos en la composici\u00f3n y densidad de los fluidos a lo largo de determinadas direcciones.  los primeros fluidos de origen, magm\u00e1tico muestran orientaciones preferentes n40-50e, los acuoso- carb\u00f3nicos ne-sw, como en la etapa anterior, n20-30e y n100e+-10 mientras que los fluidos acuosos muestran las trayectorias m\u00e1s complejas, pues en parte, aprovechan fracturas anteriores para migrar, adem\u00e1s de orientaciones tard\u00edas, como son e-w y n-s.  los resultados indican que la circulaci\u00f3n hidrotermal sucedi\u00f3 de una manera homog\u00e9nea atrav\u00e9s de una red de microfracturas interconectadas fruto de la presencia de un campo de esfuerzos regional.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Analisis de la circulacion hidrotermal en granitos mineralizados con w-sn (sierra de guadarrama).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Analisis de la circulacion hidrotermal en granitos mineralizados con w-sn (sierra de guadarrama). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Eugenia Garcia Garcia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/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>Jos\u00e9 Angel Garcia  Lopez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Mercedes Doval Montoya <\/li>\n<li>Carlos Villaseca Gonzalez (vocal)<\/li>\n<li>Jos\u00e9 Mangas Vi\u00f1uela (vocal)<\/li>\n<li>Christine Boiron Marie (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Eugenia Garcia Garcia En este trabajo se estudia la forma en que los fluidos hidrotermales asociados a [&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":[3498,27,953,3499,1666],"tags":[29855,48705,92701,76033,4038,5198],"class_list":["post-34303","post","type-post","status-publish","format-standard","hentry","category-aguas-subterraneas","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-hidrogeologia","category-hidrologia","tag-carlos-villaseca-gonzalez","tag-christine-boiron-marie","tag-eugenia-garcia-garcia","tag-jose-angel-garcia-lopez","tag-jose-mangas-vinuela","tag-mercedes-doval-montoya"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/34303","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=34303"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/34303\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=34303"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=34303"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=34303"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}