{"id":135064,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-estructura-y-evolucion-tectonoestratigrafica-del-borde-occidental-de-la-cuenca-vasco-cantabrica-cordillera-cantabrica-no-de-espana\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"la-estructura-y-evolucion-tectonoestratigrafica-del-borde-occidental-de-la-cuenca-vasco-cantabrica-cordillera-cantabrica-no-de-espana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-estructura-y-evolucion-tectonoestratigrafica-del-borde-occidental-de-la-cuenca-vasco-cantabrica-cordillera-cantabrica-no-de-espana\/","title":{"rendered":"La estructura y evolucion tectonoestratigrafica del borde occidental de la cuenca vasco-cantabrica (cordillera cantabrica – no de espa\u00f1a)."},"content":{"rendered":"

Tesis doctoral de Garcia Espina Martinez Ricardo <\/strong><\/h2>\n

A partir del levantamiento de un mapa geologico del borde occidental de la cuenca vasco cantabrica se han caracterizado las estructuras expensionales mesozoicas y las correspondientes a la deformacion alpina subsiguiente.En estratigrafia se han reorganizado parte de las unidades estratigraficas procurando que tuvieran validez en un area.Se llega a la conclusion de que los procesos extensionales se suceden en varios periodos entre permico y cretacico con intrusiones de (ceuper en fallas normales (romaceo y riocuclo) en la deformacion alpina se concentra en cuatro bandas de n. A. S. Con un acortamiento total de 21 km.<\/p>\n

 <\/p>\n

Datos acad\u00e9micos de la tesis doctoral \u00abLa estructura y evolucion tectonoestratigrafica del borde occidental de la cuenca vasco-cantabrica (cordillera cantabrica – no de espa\u00f1a).<\/strong>\u00ab<\/h3>\n
    \n
  • T\u00edtulo de la tesis:<\/strong>\u00a0 La estructura y evolucion tectonoestratigrafica del borde occidental de la cuenca vasco-cantabrica (cordillera cantabrica – no de espa\u00f1a). <\/li>\n
  • Autor:<\/strong>\u00a0 Garcia Espina Martinez Ricardo <\/li>\n
  • Universidad:<\/strong>\u00a0 Oviedo<\/li>\n
  • Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/li>\n<\/ul>\n

     <\/p>\n

    Direcci\u00f3n y tribunal<\/h3>\n
      \n
    • Director de la tesis<\/strong>\n
        \n
      • Alvarez Pulgar Francisco Javier<\/li>\n<\/ul>\n<\/li>\n
      • Tribunal<\/strong>\n
          \n
        • Presidente del tribunal: Alberto Marcos Vallaure <\/li>\n
        • Guimera Roso Joan Josep (vocal)<\/li>\n
        • Victoriano Pujalte Navarro (vocal)<\/li>\n
        • Antonio Casas Sainz (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n

           <\/p>\n","protected":false},"excerpt":{"rendered":"

          Tesis doctoral de Garcia Espina Martinez Ricardo A partir del levantamiento de un mapa geologico del borde occidental de la […]<\/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":[27,953,3435,8846],"tags":[9049,81499,126166,249234,249235,13245],"class_list":["post-135064","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-estructural","category-oviedo","tag-alberto-marcos-vallaure","tag-alvarez-pulgar-francisco-javier","tag-antonio-casas-sainz","tag-garcia-espina-Martinez-ricardo","tag-guimera-roso-joan-josep","tag-victoriano-pujalte-navarro"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/135064","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=135064"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/135064\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=135064"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=135064"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=135064"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}