{"id":139550,"date":"2026-01-12T17:46:35","date_gmt":"2026-01-12T17:46:35","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructura-geologica-de-la-region-del-mampodre-y-areas-adyacentes-zona-cantabrica\/"},"modified":"2026-01-12T17:46:35","modified_gmt":"2026-01-12T17:46:35","slug":"estructura-geologica-de-la-region-del-mampodre-y-areas-adyacentes-zona-cantabrica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estructura-geologica-de-la-region-del-mampodre-y-areas-adyacentes-zona-cantabrica\/","title":{"rendered":"\u00abestructura geologica de la region del mampodre y areas adyacentes (zona cantabrica)\u00bb."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Nemesio Heredia Carballo <\/strong><\/h2>\n<p>El area del mampodre se situa dentro de la zona cantabrica, la mas externa desde el punto de vista estructural de la cordillera varisca del no peninsular.  dentro de la zona cantabrica la zona estudiada se enmarca en las unidades del ponga, cuenca carbonifera central y pisuerga-carrion (julivert, 1971).  desde el punto de vista estratigrafico se caracteriza por presentar un paleozoico inferior muy reducido de edad cambro-ordovicico sobre el que se apoya una potente serie carbonifera constituida en su mayor parte por el grupo lena (namuriense-westfaliense) en la cuenca carbonifera central y unidad del ponga y por los grupos prioro, pando, mara\u00f1a, ponton, valdeon y remo\u00f1a en la unidad del pisuerga-carrion comprendidos entre el namuriense y el estefaniense b.  desde el punto de vista estructural se caracteriza por un predominio de la tectonica tangencial, donde los cabalgamientos y pliegues asociados son las estructuras predominantes, abundando las geometrias de tipo duplex.  estos cabalgamientos se han emplazado entre el westfaliense d superior y el barrueliense (estefaniense a).<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>\u00abestructura geologica de la region del mampodre y areas adyacentes (zona cantabrica)\u00bb.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 \u00abestructura geologica de la region del mampodre y areas adyacentes (zona cantabrica)\u00bb. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Nemesio Heredia Carballo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1992<\/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>Andres Perez Estaun<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jaime Truyols Santonja <\/li>\n<li> Casas Tuset Josep M. (vocal)<\/li>\n<li>Manuel Julivert Casagualda (vocal)<\/li>\n<li>Francisco Gonzalez Lodeiro (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Nemesio Heredia Carballo El area del mampodre se situa dentro de la zona cantabrica, la mas externa [&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":[27,245,953,3435,8846],"tags":[9050,116045,21742,25246,21743,51165],"class_list":["post-139550","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-estratigrafia","category-geologia","category-geologia-estructural","category-oviedo","tag-andres-perez-estaun","tag-casas-tuset-josep-m","tag-francisco-gonzalez-lodeiro","tag-jaime-truyols-santonja","tag-manuel-julivert-casagualda","tag-nemesio-heredia-carballo"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139550","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=139550"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139550\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=139550"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=139550"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=139550"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}