{"id":80618,"date":"2018-03-10T00:04:23","date_gmt":"2018-03-10T00:04:23","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-estructura-de-la-sierra-de-cameros-deformacion-ductil-y-su-significado-a-escala-cortical\/"},"modified":"2018-03-10T00:04:23","modified_gmt":"2018-03-10T00:04:23","slug":"la-estructura-de-la-sierra-de-cameros-deformacion-ductil-y-su-significado-a-escala-cortical","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-estructura-de-la-sierra-de-cameros-deformacion-ductil-y-su-significado-a-escala-cortical\/","title":{"rendered":"La estructura de la sierra de cameros: deformacion ductil y su significado a escala cortical."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Andres Gil Imaz <\/strong><\/h2>\n<p>En esta tesis se aborda el estudio, a todas las escalas, de la estructura adquirida por las rocas que constituyen el conjunto orogr\u00e1fico y geol\u00f3gico de las sierras de cameros, durante el desarrollo de los procesos deformativos mesozoicos y terciarios. Un aspecto prioritario ser\u00e1 el an\u00e1lisis del significado estructural de la deformaci\u00f3n d\u00factil en toda la cadena. los principales apartados tem\u00e1ticos desarrollados en esta tesis son los siguientes:  1) aplicaci\u00f3n de los m\u00e9todos del an\u00e1lisis de la deformaci\u00f3n finita a escala micro y mesoestructural, a las rocas jur\u00e1sicas y cret\u00e1cicas (facies purbeck-weald) del dominio de las sierras de cameros.  2) determinaci\u00f3n de la anisotrop\u00eda de susceptibilidad magn\u00e9tica (asm) en rocas de distinto grado de deformaci\u00f3n y contrastaci\u00f3n de los resultados con el an\u00e1lisis de la deformaci\u00f3n finita.  3) integraci\u00f3n de los resultados del estudio de la deformaci\u00f3n en superficie y los de profundidad, basados en la s\u00edsmica de reflexi\u00f3n.  4) estudio de la relaci\u00f3n entre la deformaci\u00f3n y el metamorfismo t\u00e9rmico de bajo grado que afecta a las rocas de este dominio.  5) dataci\u00f3n relativa de acontecimientos tect\u00f3nicos causantes de la deformaci\u00f3n de los materiales estudiados a partir de las fases minerales adecuadas, involucradas en la deformaci\u00f3n.  6) elaboraci\u00f3n de un modelo tect\u00f3nico, cinem\u00e1tico y din\u00e1mico del dominio de las sierras de cameros para el periodo mesozoico-terciario, que integra los resultados del an\u00e1lisis estructural, la anisotrop\u00eda de susceptibilidad magn\u00e9tica, el metamorfismo de bajo grado y la geof\u00edsica.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La estructura de la sierra de cameros: deformacion ductil y su significado a escala cortical.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La estructura de la sierra de cameros: deformacion ductil y su significado a escala cortical. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Andres Gil Imaz <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 16\/09\/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>Andr\u00e9s Pocovi Juan<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: pere Santanach prat <\/li>\n<li>felix Perez lorente (vocal)<\/li>\n<li> Simon gomez Jos\u00e9 Luis (vocal)<\/li>\n<li>Jos\u00e9 Manuel Gonz\u00e1lez casado (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Andres Gil Imaz En esta tesis se aborda el estudio, a todas las escalas, de la estructura [&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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