{"id":41304,"date":"1999-01-01T00:00:00","date_gmt":"1999-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-tectonica-reciente-de-la-cordillera-iberica-cuenca-del-ebro-y-pirineo-centro-occidental\/"},"modified":"1999-01-01T00:00:00","modified_gmt":"1999-01-01T00:00:00","slug":"evolucion-tectonica-reciente-de-la-cordillera-iberica-cuenca-del-ebro-y-pirineo-centro-occidental","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evolucion-tectonica-reciente-de-la-cordillera-iberica-cuenca-del-ebro-y-pirineo-centro-occidental\/","title":{"rendered":"Evolucion tectonica reciente de la cordillera iberica, cuenca del ebro y pirineo centro-occidental."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Angel Luis Cortes Gracia <\/strong><\/h2>\n<p>La evoluci\u00f3n tect\u00f3nica reciente del ne de la pen\u00ednsula ib\u00e9rica est\u00e1 caracterizada por la heterogeneidad tanto de las estructuras presentes como de las direcciones de esfuerzos tect\u00f3nicos que se pueden inferir a partir de las mismas.  macroestructura  el origen de las fosas ne\u00f3genas de la sierra de cantabria ha sido interpretado en relaci\u00f3n con la reactivaci\u00f3n reciente de los pliegues situados en el bloque superior del frente cabalgante. En las cuencas de antepa\u00eds (ebro y duero) aparecen algunas macroestructuras comprensivas y distensivas de dimensiones hectom\u00e9tricas a kilom\u00e9tricas con desniveles estructurales m\u00e9tricos a hectom\u00e9tricos. Las cuencas interiores de la cordillera ib\u00e9rica se caracterizan por la presencia de fallas normales de dimensiones kilom\u00e9tricas y salto m\u00e9trico a hectom\u00e9trico. Destacan las fallas de concud y val de la sabina, con m\u00e1s de 300 m de salto vertical. En la fosa de teruel se ha determinado la existencia de pliegues y basculamientos importantes a partir del an\u00e1lisis de superficies de referencia estratigr\u00e1ficas.  fracturacion a escala cartografica (lineamientos)  el estudio de im\u00e1genes de sat\u00e9lite ha permitido identificar m\u00e1s de 20000 lineamientos (unos 15000 en materiales recientes). Las orientaciones dominantes son: ne-sw a ene-wsw (moda principal), n-s, nw-se y e-w. En la localizaci\u00f3n y orientaci\u00f3n de las fracturas ha jugado un papel importante la existencia de estructuras previas.  estados de esfuerzos recientes  el an\u00e1lisis mesoestructural (119 nuevas estaciones en materiales recientes) ha puesto de manifiesto la existencia de estados de esfuerzos compresivos, de desgarre y distensivos, dominando estos \u00faltimos a escala regional. Las direcciones dominantes del esfuerzo horizontal m\u00e1ximo son: nne-ssw a ne-sw (moda principal), nw-se y n-s. El origen de los estados de esfuerzos est\u00e1 relacionado con las fuerzas producidas en los bordes de colisi\u00f3n de la placa<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evolucion tectonica reciente de la cordillera iberica, cuenca del ebro y pirineo centro-occidental.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evolucion tectonica reciente de la cordillera iberica, cuenca del ebro y pirineo centro-occidental. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Angel Luis Cortes Gracia <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/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> Casas Sainz Antonio  M.<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: pere Santanach prat <\/li>\n<li> De vicente mu\u00f1oz gerardo (vocal)<\/li>\n<li> Martinez pe\u00f1a m. bego\u00f1a (vocal)<\/li>\n<li>claudio Faccenna (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Angel Luis Cortes Gracia La evoluci\u00f3n tect\u00f3nica reciente del ne de la pen\u00ednsula ib\u00e9rica est\u00e1 caracterizada por [&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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