{"id":71722,"date":"2004-10-12T00:00:00","date_gmt":"2004-10-12T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-sedimentologia-y-evolucion-tectonosedimentaria-de-las-sucesiones-estefanienses-de-la-region-de-picos-de-europa-zona-cantabrica\/"},"modified":"2004-10-12T00:00:00","modified_gmt":"2004-10-12T00:00:00","slug":"estratigrafia-sedimentologia-y-evolucion-tectonosedimentaria-de-las-sucesiones-estefanienses-de-la-region-de-picos-de-europa-zona-cantabrica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-sedimentologia-y-evolucion-tectonosedimentaria-de-las-sucesiones-estefanienses-de-la-region-de-picos-de-europa-zona-cantabrica\/","title":{"rendered":"Estratigrafia, sedimentolog\u00eda y evolucion tectonosedimentaria de las sucesiones estefanienses de la region de picos de europa (zona cantabrica)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Oscar Antonio Merino Tome <\/strong><\/h2>\n<p>La regi\u00f3n de picos de europa es la unidad tectonoestratigr\u00e1fica m\u00e1s interna de la zona cant\u00e1brica (no del macizo ib\u00e9rico). Durante el bashkiriense y el moscoviense (carbon\u00edfero superior) constituy\u00f3 un dominio distal de la cuenca de antepa\u00eds varisca en el que se desarroll\u00f3 una extensa plataforma carbonatada con m\u00e1rgenes elevados (formaciones picos de europa y valdeteja). desde el moscoviense superior (myachkovsky superior) hasta el gzheliense esta plataforma carbonatada fue progresivamente incorporada a la cu\u00f1a orog\u00e9nica y compartimentada en un conjunto de escamas de cabalgamiento de direcci\u00f3n e-o emplazadas hacia el s mientras se produc\u00eda el cierre del arco art\u00farico.  en este contexto se desarrollaron nuevas cuencas tect\u00f3nicamente activas y fuertemente subsidentes cuyo relleno est\u00e1 integrado por dep\u00f3sitos cl\u00e1sticos gruesos (brechas calc\u00e1reas y megabrechas, conglomerados y calclititas), areniscas, lutitas, margas y calizas. Dichos materiales registran la evoluci\u00f3n tect\u00f3nica y el proceso de construcci\u00f3n de la cu\u00f1a orog\u00e9nica, as\u00ed como la compleja interacci\u00f3n de entre la actividad tect\u00f3nica y las variaciones glacio-eust\u00e1ticas del nivel del mar en las cuencas desarrolladas sobre ella.  esta tesis doctoral afronta el estudio cartogr\u00e1fico, estratigr\u00e1fico y sedimentol\u00f3gico conjunto de las sucesiones sinorog\u00e9nicas estefanieses para conocer la configuraci\u00f3n de las cuencas donde se acumularon y los procesos geol\u00f3gicos aloc\u00edclicos que controlaron la arquitectura de su relleno sedimentario y evoluci\u00f3n. La informaci\u00f3n obtenida permite establecer un modelo general de evoluci\u00f3n de la regi\u00f3n de picos de europa y de las \u00e1reas adyacentes de la zona cant\u00e1brica y el proceso de construcci\u00f3n de la cu\u00f1a orog\u00e9nica durante las \u00faltimas fases de la orogenia varisca en el carbon\u00edfero superior.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia, sedimentolog\u00eda y evolucion tectonosedimentaria de las sucesiones estefanienses de la region de picos de europa (zona cantabrica)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia, sedimentolog\u00eda y evolucion tectonosedimentaria de las sucesiones estefanienses de la region de picos de europa (zona cantabrica) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Oscar Antonio Merino Tome <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 10\/12\/2004<\/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>Juan  Ramon Colmenero Navarro<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Antonio Vera torres <\/li>\n<li> Alonso alonso  Juan  Luis (vocal)<\/li>\n<li>lorenzo Vilas minondo (vocal)<\/li>\n<li>elisa Villa otero (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Oscar Antonio Merino Tome La regi\u00f3n de picos de europa es la unidad tectonoestratigr\u00e1fica m\u00e1s interna de [&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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