{"id":48260,"date":"2020-09-05T22:31:07","date_gmt":"2020-09-05T22:31:07","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-y-estructura-del-domo-de-lugo-sector-oeste-de-la-zona-asturoccidental-leonesa\/"},"modified":"2020-09-05T22:31:07","modified_gmt":"2020-09-05T22:31:07","slug":"estratigrafia-y-estructura-del-domo-de-lugo-sector-oeste-de-la-zona-asturoccidental-leonesa","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-y-estructura-del-domo-de-lugo-sector-oeste-de-la-zona-asturoccidental-leonesa\/","title":{"rendered":"Estratigrafia y estructura del domo de lugo (sector oeste de la zona asturoccidental-leonesa)"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Martinez Catalan Jos\u00e9 Ramon <\/strong><\/h2>\n<p>El sector estudiado incluye rocas paleozoicas y precambricas que forman parte de una importante estructura aloctona  el manto de mondo\u00f1edo  asi como rocas de similar edad que forman su autoctono relativo.  los materiales autoctonos afloran en dos ventanas tectonicas que coinciden con sendos domos producidos por interferencia de dos sistemas de pliegues superpuestos.  se ha realizado una correlacion litoestratigrafica entre los materiales del manto y los de su autoctono y se han analizado las estructuras producidas por los diferentes episodios de deformacion  de los cuales se han identificado cinco: los dos primeros caracteristicos de una tectonica tangencial  el tercero da una falla normal y los dos ultimos repliegan las estructuras previas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia y estructura del domo de lugo (sector oeste de la zona asturoccidental-leonesa)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia y estructura del domo de lugo (sector oeste de la zona asturoccidental-leonesa) <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Martinez Catalan Jos\u00e9 Ramon <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1981<\/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>Florencio Aldaya Valverde<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Florencio Aldaya Valverde <\/li>\n<li>Victor Garcia Due\u00f1as (vocal)<\/li>\n<li>Manuel Julivert Casagualda (vocal)<\/li>\n<li>Alberto Marcos Vallaure (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Martinez Catalan Jos\u00e9 Ramon El sector estudiado incluye rocas paleozoicas y precambricas que forman parte de 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 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