{"id":84261,"date":"2018-03-10T00:08:29","date_gmt":"2018-03-10T00:08:29","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/fracturacion-y-campos-de-esfuerzos-compresivos-alpinos-en-la-cordillera-iberica-y-el-ne-peninsular\/"},"modified":"2018-03-10T00:08:29","modified_gmt":"2018-03-10T00:08:29","slug":"fracturacion-y-campos-de-esfuerzos-compresivos-alpinos-en-la-cordillera-iberica-y-el-ne-peninsular","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/fracturacion-y-campos-de-esfuerzos-compresivos-alpinos-en-la-cordillera-iberica-y-el-ne-peninsular\/","title":{"rendered":"Fracturaci\u00f3n y campos de esfuerzos compresivos alpinos en la cordillera ib\u00e9rica y el ne peninsular"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Carlos Luis Liesa Carrera <\/strong><\/h2>\n<p>El estudio comparado de la fracturaci\u00f3n a las escalas macro-, meso-, y microestructural en tres sectores de la cordillera ib\u00e9rica centro-oriental (sectores de mosqueruela, la siera de camarena y la sierra del pobo) ha permitido distinguir dos patrones de fracturaci\u00f3n distintos.  el primero, representado en los materiales de jur\u00e1sico y cret\u00e1cico inferior de las sierras de camarena y el pobo, est\u00e1 determinado por cuatro familias de fracturas de direcciones ne-so, no-se (nno-sse en el pobo), e-o y n-s. son en su mayor\u00eda fallas normales y diaclasas formadas en condiciones extensionales durante dos episodios distintos del rifting jur\u00e1sico superior-cret\u00e1ctico inferior.  el segundo patr\u00f3n de fracturaci\u00f3n, representado en las calizas del cret\u00e1cico superior del sector de mosqueruela, es sensiblemente m\u00e1s sencillo, y est\u00e1 compuesto por tres familias de fallas direccionales (nne, ene y ese) formadas durante las etapas compresivas terciarias. El an\u00e1lisis de los estados de esfuerzos puntuales registrados en estos sectores en relaci\u00f3n con las estructuras de su alrededor nos ha permitido concluir que los estados de esfuerzos inferidos a partir de datos de afloramiento representan con bastante fiabilidad el campo de esfuerzos primario y adem\u00e1s permiten caracterizar c\u00f3mo act\u00faa \u00e9ste en relaci\u00f3n con las macroestructuras previas.  los resultados obtenidos en los tres sectores estudiados, as\u00ed como los procedentes de la recopilaci\u00f3n de todos los estados de esfuerzos compresivos registrados en la cordillera ib\u00e9rica y su entorno y su an\u00e1lisis exhaustivo sobre el mapa geol\u00f3gico, han permitido caracterizar tres campos de esfuerzos compresivos intraplaca distintos, los cuales hna determinado la evoluci\u00f3n terciaria del ne peninsular: campos de esfuerzos compresivos ib\u00e9rico (-1 ne-so), b\u00e9tico s.L.(-1 medio no-se) y perinaico (-1 n a nne). La direcci\u00f3n de compresi\u00f3n en el campo b\u00e9tico s.L.Evoluci\u00f3n en el tiempo (giro horario de -1) d<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Fracturaci\u00f3n y campos de esfuerzos compresivos alpinos en la cordillera ib\u00e9rica y el ne peninsular<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Fracturaci\u00f3n y campos de esfuerzos compresivos alpinos en la cordillera ib\u00e9rica y el ne peninsular <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Carlos Luis Liesa Carrera <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 14\/04\/2000<\/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> Sim\u00f3n G\u00f3mez Jos\u00e9 Luis<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: ramon Capote del villar <\/li>\n<li> De vicente mu\u00f1oz gerardo (vocal)<\/li>\n<li>joan Guimera rosso (vocal)<\/li>\n<li> Casas sainz Antonio  m. (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Carlos Luis Liesa Carrera El estudio comparado de la fracturaci\u00f3n a las escalas macro-, meso-, y microestructural [&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":[27,178100,1033,953,3435,19202,20496,13610],"tags":[178101,74307,104703,34044,6703,73593],"class_list":["post-84261","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-fotogeologia","category-geofisica","category-geologia","category-geologia-estructural","category-geologia-regional","category-tectonica","category-zaragoza","tag-carlos-luis-liesa-carrera","tag-casas-sainz-antonio-m","tag-de-vicente-munoz-gerardo","tag-joan-guimera-rosso","tag-ramon-capote-del-villar","tag-simon-gomez-jose-luis"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/84261","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=84261"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/84261\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=84261"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=84261"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=84261"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}