{"id":81667,"date":"2018-03-10T00:05:33","date_gmt":"2018-03-10T00:05:33","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-metamorfismo-de-la-sierra-de-camerosla-rioja-espana-petrologa%c2%ada-geoqua%c2%admica-geocronologa%c2%ada-y-contexto-estructural-de-los-procesos-de-interaccion-fluido-roca\/"},"modified":"2018-03-10T00:05:33","modified_gmt":"2018-03-10T00:05:33","slug":"el-metamorfismo-de-la-sierra-de-camerosla-rioja-espana-petrologa%c2%ada-geoqua%c2%admica-geocronologa%c2%ada-y-contexto-estructural-de-los-procesos-de-interaccion-fluido-roca","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-metamorfismo-de-la-sierra-de-camerosla-rioja-espana-petrologa%c2%ada-geoqua%c2%admica-geocronologa%c2%ada-y-contexto-estructural-de-los-procesos-de-interaccion-fluido-roca\/","title":{"rendered":"El metamorfismo de la sierra de cameros(la rioja, espa\u00f1a): petrolog\u00eda, geoqu\u00edmica, geocronolog\u00eda y contexto estructural de los procesos de interacci\u00f3n fluido-roca."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Mantilla Figueroa Luis Carlos <\/strong><\/h2>\n<p>La presente tesis doctoral, realizada en la cuenca de cameros (la rioja, espa\u00f1a), ha abordado, esencialmente, la problem\u00e1tica relacionada con el metomorfismo que ha afectado la cuenca con posterioridad a su relleno.  la investigaci\u00f3n realizada entorno a esta problem\u00e1tica, se desarroll\u00f3 estudiando la naturaleza petrogr\u00e1fica, geoqu\u00edmica (mayores, menores, tierras raras, estables y radiog\u00e9nicos), termocronol\u00f3gica y rasgos estructurales, tanto del sector afectado por el metamorfismo, como de sus sectores circunvecinos. esta tarea, permiti\u00edo identificar y contextualizar los procesos de interacci\u00f3n fluido-roca, que tuvieron lugar durante la evoluci\u00f3n de la cuenca.  los resultados de esta investigaci\u00f3n, validan el modelo de metamorfismo hidrotermal y aportan argumentos, desde esta perspectiva, sobre:1) la presencia de una clara inversi\u00f3n termal; 2) la procedencia al\u00f3ctona de los solutos constituyentes de los fluidos, que participaron en la alteraci\u00f3n hidrotermal; 3) la modificaci\u00f3n qu\u00edmica de las rocas, como consecuencia del car\u00e1cter aloqu\u00edmico del metamorfismo; y 4) la estrecha relaci\u00f3n entre las estructuras de deformaci\u00f3n (esquistosidad) y los fluidos calientes migratorios; entre otros varios aspectos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El metamorfismo de la sierra de cameros(la rioja, espa\u00f1a): petrolog\u00eda, geoqu\u00edmica, geocronolog\u00eda y contexto estructural de los procesos de interacci\u00f3n fluido-roca.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El metamorfismo de la sierra de cameros(la rioja, espa\u00f1a): petrolog\u00eda, geoqu\u00edmica, geocronolog\u00eda y contexto estructural de los procesos de interacci\u00f3n fluido-roca. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Mantilla Figueroa Luis Carlos <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 15\/12\/1999<\/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>C\u00e9sar Casquet Mart\u00edn<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: rafaela Marfil perez <\/li>\n<li>Jos\u00e9 Manuel Gonz\u00e1lez casado (vocal)<\/li>\n<li>magdalena Rodas gonzalez (vocal)<\/li>\n<li>angela Alonso millan (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Mantilla Figueroa Luis Carlos La presente tesis doctoral, realizada en la cuenca de cameros (la rioja, espa\u00f1a), [&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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