{"id":13992,"date":"2018-03-09T09:00:30","date_gmt":"2018-03-09T09:00:30","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-pluton-de-patincosa-huesca-pirineos-estructura-y-modelo-de-emplazamiento-a-partir-del-analisis-de-la-anisotropia-de-la-susceptibilidad-magnetica\/"},"modified":"2018-03-09T09:00:30","modified_gmt":"2018-03-09T09:00:30","slug":"el-pluton-de-patincosa-huesca-pirineos-estructura-y-modelo-de-emplazamiento-a-partir-del-analisis-de-la-anisotropia-de-la-susceptibilidad-magnetica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-pluton-de-patincosa-huesca-pirineos-estructura-y-modelo-de-emplazamiento-a-partir-del-analisis-de-la-anisotropia-de-la-susceptibilidad-magnetica\/","title":{"rendered":"El plut\u00f3n de patincosa (huesca, pirineos): estructura y modelo de emplazamiento a partir del an\u00e1lisis de la anisotropia de la susceptibilidad magn\u00e9tica."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Santana Torres Vicente Jos\u00e9 <\/strong><\/h2>\n<p>El macizo gran\u00edtico de panticosa (valle de tena, huesca) es un plut\u00f3n de geometr\u00eda concentrica (40 km2) que aflora en un \u00e1rea de alta monta\u00f1a en la zona axial de los pirineos. Este plut\u00f3n de edad herc\u00ednica se emplaza en materiales sedimentarios del paleozoico superior, fundamentalmente dev\u00f3nicos. consta de cuatro facies petrogr\u00e1ficas dispuestas de zonaci\u00f3n concentrica normal: monzogranito (facies central), granodiorita clara y oscura y gabrodioritas (facies externa). La transici\u00f3n entre los diferentes tipos litol\u00f3gicos se produce de forma gradual.  su estructura interna se ha obtenido aplicando t\u00e9cnicas cl\u00e1sicas de geolog\u00eda estructural y mediante la t\u00e9cnica de la anisotrop\u00eda de la susceptibilidad magn\u00e9tica (98 estaciones de sondeo). La estructura interna del plut\u00f3n muestra una geometr\u00eda singmoide que corta claramente a la zonaci\u00f3n petrogr\u00e1fica. el car\u00e1cter paramagn\u00e9tico de \u00e9stas rocas, ha permitido conseguir una correlaci\u00f3n perfecta entre el tipo petrogr\u00e1fico y el valor de la susceptibilidad magn\u00e9tica, con lo que se ha logrado detallar a\u00fan m\u00e1s la zonaci\u00f3n petrogr\u00e1fica. El estudio microestructural muestra que la estructura interna se ha adquirido mayoritariamente en estado magm\u00e1tico, sin embargo en el borde noroeste se concentran los valores m\u00e1s altos de anisotrop\u00eda (p%) coincidiendo espacialmente con el dominio donde aparecen las microestructuras de deformaci\u00f3n en estado s\u00f3lido de alta temperatura.  el desarrollo gradual  de las microestructuras, desde magm\u00e1ticas hasta de deformaci\u00f3n en estado s\u00f3lido, y la continuidad de las f\u00e1bricas asociadas a \u00e9stas, sugieren que  la adquisici\u00f3n de la f\u00e1brica comienza durante la cristalizaci\u00f3n del magma y contin\u00faa durante los primeros estadios del enfrentamiento \u00absubs\u00f3lidus\u00bb del plut\u00f3n.  el modelo propuesto cotempla el emplazamiento sincinem\u00e1tico del plut\u00f3n de panticosa en la corteza superior fr\u00e1gil, como un proceso de deformaci\u00f3n progresivo y contin<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El plut\u00f3n de patincosa (huesca, pirineos): estructura y modelo de emplazamiento a partir del an\u00e1lisis de la anisotropia de la susceptibilidad magn\u00e9tica.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El plut\u00f3n de patincosa (huesca, pirineos): estructura y modelo de emplazamiento a partir del an\u00e1lisis de la anisotropia de la susceptibilidad magn\u00e9tica. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Santana Torres Vicente Jos\u00e9 <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Pa\u00eds vasco\/euskal herriko unibertsitatea<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 23\/11\/2001<\/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>Aitor Aranguren Iriarte<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Tub\u00eda mart\u00ednez Jos\u00e9 Mar\u00eda <\/li>\n<li>g\u00e9rad Gleizes (vocal)<\/li>\n<li> Mart\u00ednez catal\u00e1n Jos\u00e9 ram\u00f3n (vocal)<\/li>\n<li>Fernando Alvarez lobato (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Santana Torres Vicente Jos\u00e9 El macizo gran\u00edtico de panticosa (valle de tena, huesca) es un plut\u00f3n 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 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