{"id":80996,"date":"2018-03-10T00:04:48","date_gmt":"2018-03-10T00:04:48","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructura-y-evolucion-alpina-de-la-cuenca-de-almazan-cordillera-iberica\/"},"modified":"2018-03-10T00:04:48","modified_gmt":"2018-03-10T00:04:48","slug":"estructura-y-evolucion-alpina-de-la-cuenca-de-almazan-cordillera-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estructura-y-evolucion-alpina-de-la-cuenca-de-almazan-cordillera-iberica\/","title":{"rendered":"Estructura y evoluci\u00f3n alpina de la cuenca de almaz\u00e1n (cordillera ib\u00e9rica)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Adolfo Maestro Gonz\u00e1lez <\/strong><\/h2>\n<p>La cuenca de almaz\u00e1n se sit\u00faa al norte de la pen\u00ednsula ib\u00e9rica. Presenta una geometr\u00eda sinclinal de charnela plana de orientaci\u00f3n nw-se a e-w. El margen septentrional muestra un sistema de cabalgamientos vergentes al sur de orientaci\u00f3n e-w a wnw-ese. El borde de oriental limita con la rama aragonesa cuya estructura puede explicarse como resultado de la reactivaci\u00f3n de la estructura herc\u00ednica. Las estructuras de borde meridional (rama castellana) son de orientaci\u00f3n e-w. Los dep\u00f3sitos terciarios, con un espesor de unos 3500 m, est\u00e1n constituidos por cuatro unidades tectosedimentarias pale\u00f3genas (eoceno-ageniense), y los materiales ne\u00f3genos (ageniense-plioceno) se disponen subhorizontales. Las principales estructuras contempor\u00e1neas con el dep\u00f3sito de los materiales terciarios son los monoclinales de almaz\u00e1n, de arcos y de g\u00f3mara. El desplazamiento del cabalgamiento de cameros hacia el norte implica el transporte de la cuenca de almz\u00e1n, fundamentalmente durante el eoceno superior-oligoceno superior. En este sentido la cuenca de almaz\u00e1n se puede considerar como una cuenca de piggy-back asociada a un cabalgamiento de escala cortical.  las direcciones de compresi\u00f3n terciarias son: nne-ssw, nw-se, ne-sw y e-w. Se pude interpretar que la direcci\u00f3n de o-1 del campo de esfuerzos primario es nne-ssw que parece desviada por grandes estructuras que se reactivaron como direccionales-inversas. Durante el mioceno superior-plioceno domina un campo de esfuerzos distensivo, con direcciones de o3: ese a se y ne-sw.  en los materiales pale\u00f3genos las fracturas se sit\u00faan paralelas y perpendiculares a los ejes de los pliegues. Gen\u00e9ticamente est\u00e1n relacionadas con el campo compresivo nne a ne, y a la evoluci\u00f3n de los pliegues. En el sector central y oriental de la cuenca (materiales ne\u00f3genos) la direcci\u00f3n de fracturaci\u00f3n es ne-sw, nw-se y e-w.La imagen sat\u00e9lite muestra una orientaci\u00f3n de los lineamientos ene-wsw. Esta puede ser deb<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estructura y evoluci\u00f3n alpina de la cuenca de almaz\u00e1n (cordillera ib\u00e9rica)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estructura y evoluci\u00f3n alpina de la cuenca de almaz\u00e1n (cordillera ib\u00e9rica) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Adolfo Maestro Gonz\u00e1lez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 22\/10\/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>Antonio Casas Sainz<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: javier Alvarez pulgar <\/li>\n<li>Andr\u00e9s Pocovi Juan (vocal)<\/li>\n<li>Jos\u00e9 Manuel Gonz\u00e1lez casado (vocal)<\/li>\n<li>Jes\u00fas Galindo zaldivar (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Adolfo Maestro Gonz\u00e1lez La cuenca de almaz\u00e1n se sit\u00faa al norte de la pen\u00ednsula ib\u00e9rica. Presenta una [&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":[27,953,3435,75,13610],"tags":[173083,66240,126166,127809,73592,39091],"class_list":["post-80996","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-estructural","category-geomorfologia","category-zaragoza","tag-adolfo-maestro-gonzalez","tag-andres-pocovi-juan","tag-antonio-casas-sainz","tag-javier-alvarez-pulgar","tag-jesus-galindo-zaldivar","tag-jose-manuel-gonzalez-casado"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/80996","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=80996"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/80996\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=80996"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=80996"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=80996"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}