{"id":82283,"date":"2000-01-01T00:00:00","date_gmt":"2000-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-relieve-de-los-paramos-de-la-lora\/"},"modified":"2000-01-01T00:00:00","modified_gmt":"2000-01-01T00:00:00","slug":"el-relieve-de-los-paramos-de-la-lora","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-relieve-de-los-paramos-de-la-lora\/","title":{"rendered":"El relieve de los paramos de la lora."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Gutierrez Nevado Dionisio Javier <\/strong><\/h2>\n<p>En este trabajo se estudia el relieve de los p\u00e1ramos de la lora en el sector meridional de la cordillera cant\u00e1brica, zona centro oriental. Se analizan las morfoestructuras, la red hidrogr\u00e1fica y los modelados fluvial y c\u00e1rstico, intentando llegar a un esquema evolutivo de la g\u00e9nesis del relieve.  la zona se articula como un sinclinal colgado complejo articulado por materiales calc\u00e1reos que han quedado en resalte por la disecci\u00f3n morfoest\u00e1tica del valle de valderredible al norte (r\u00edos ebro y mardancho) y por la disecci\u00f3n morfotect\u00f3nica del valle lucio-tozo-urbel al sur.  la g\u00e9nesis y evoluci\u00f3n del relieve se puede sistematizar as\u00ed:  1) superficie de erosi\u00f3n intramiocena  2) deformaci\u00f3n morfotect\u00f3nica en el sur (valle lucio-tozo-urbel) y levantamiento de la cresta de corral nuevo y el bloque de mu\u00f1ata, lo que provoca la reorganizaci\u00f3n de la red hidrogr\u00e1fica.  3) secuencia de disecci\u00f3n principal que deja en resalte las morfoestructuras y origina los modelados fluviales y c\u00e1rsticos.#<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El relieve de los paramos de la lora.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El relieve de los paramos de la lora. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Gutierrez Nevado Dionisio Javier <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/2000<\/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>Casildo Ferreras Chasco<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jes\u00fas Garcia fernandez <\/li>\n<li> Moreno pe\u00f1a Jos\u00e9 Luis (vocal)<\/li>\n<li>guillermo Meaza rodriguez (vocal)<\/li>\n<li> Garcia codron Juan  Carlos (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gutierrez Nevado Dionisio Javier En este trabajo se estudia el relieve de los p\u00e1ramos de la lora [&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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