{"id":6892,"date":"1995-01-01T00:00:00","date_gmt":"1995-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1995\/01\/01\/la-estructura-geologica-del-valle-del-trubia-zona-cantabrica-no-de-espana\/"},"modified":"1995-01-01T00:00:00","modified_gmt":"1995-01-01T00:00:00","slug":"la-estructura-geologica-del-valle-del-trubia-zona-cantabrica-no-de-espana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-estructura-geologica-del-valle-del-trubia-zona-cantabrica-no-de-espana\/","title":{"rendered":"La estructura geologica del valle del trubia (zona cantabrica no de espa\u00f1a)"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Bulnes Cudeiro M. Teresa <\/strong><\/h2>\n<p>La zona estudiada se situa en la zona cantabrica, que corresponde a la parte externa del orogeno hercinico del no de la peninsula iberica. La practica totalidad de las rocas existentes en el area cartografiada pertenecen a la era paleozoica. Desde el punto de vista estructural, la macroestructura de la region estudiada consiste en cuatro grandes pliegues longitudinales, dos anticlinales y dos sinclinales. Otras estructuras importantes que se observan en el mapa son los cabalgamientos. Pliegues y cabalgamientos estan relacionados geneticamente, y se observan numerosos ejemplos del paso de cabalgamientos a pliegues.  la posicion de los indicadores cinematicos, si bien indica una direccion general de transporte tectonico hacia el e, cambia de direccion de s. A n en el sentido de las agujas del reloj, orientandose segun tres direcciones preferentes. Esta particular disposicion es debida total o parcialmente a una deformacion posterior al emplazamiento de las principales estructuras.  el acortamiento minimo producido por las estructuras presentes en la zona estudiada oscilan entre el 56,9% y el 59,4%.  la construccion de un corte desde el antiforme del narcea hasta la cuenca carbonifera central, y la seccion restituida del mismo, permite tener una vision de conjunto, actualizada, de la parte n de las unidades mas occidentales de la zona cantabrica. Se ponen de manifiesto variaciones estructurales segun una direccion o-e, por ejemplo en la geometria que presentan los pliegues y los cabalgamientos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La estructura geologica del valle del trubia (zona cantabrica no de espa\u00f1a)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La estructura geologica del valle del trubia (zona cantabrica no de espa\u00f1a) <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Bulnes Cudeiro M. Teresa <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1995<\/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>Alberto Marcos Vallaure<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Victor Garcia Due\u00f1as <\/li>\n<li>Andr\u00e9s Perez Estaun (vocal)<\/li>\n<li>Jenaro Luis Garcia Alcalde Fernandez (vocal)<\/li>\n<li> Arboleya Cimadevilla M. Luisa (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Bulnes Cudeiro M. Teresa La zona estudiada se situa en la zona cantabrica, que corresponde a la [&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":[27,953,3435,19202,8846],"tags":[9049,9050,25264,25263,9315,3438],"class_list":["post-6892","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-estructural","category-geologia-regional","category-oviedo","tag-alberto-marcos-vallaure","tag-andres-perez-estaun","tag-arboleya-cimadevilla-m-luisa","tag-bulnes-cudeiro-m-teresa","tag-jenaro-luis-garcia-alcalde-fernandez","tag-victor-garcia-duenas"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/6892","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=6892"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/6892\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=6892"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=6892"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=6892"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}