{"id":142821,"date":"1993-01-01T00:00:00","date_gmt":"1993-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/geomorfologia-del-area-de-contacto-del-sistema-central-con-la-cuenca-del-duero-entre-los-rios-adaja-y-tormes\/"},"modified":"1993-01-01T00:00:00","modified_gmt":"1993-01-01T00:00:00","slug":"geomorfologia-del-area-de-contacto-del-sistema-central-con-la-cuenca-del-duero-entre-los-rios-adaja-y-tormes","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geomorfologia-del-area-de-contacto-del-sistema-central-con-la-cuenca-del-duero-entre-los-rios-adaja-y-tormes\/","title":{"rendered":"Geomorfolog\u00eda del area de contacto del sistema central con la cuenca del duero entre los rios adaja y tormes"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Miguel Herrero Matias <\/strong><\/h2>\n<p>El trabajo presenta el estudio geomorfologico del sector de zocalo (granitico) que se identifica con la sierra de avila. La investigacion se ha desarrollado mediante la aplicacion de una metodolog\u00eda de caracter inductivo y cartografico. Objetivos: 1.- Formacion de una cartografia geomorfologica de detalle. 2.- Definicion de las unidades morfoestructurales. 3.- Catalogacion de las formas del relieve. 4.- Elaboracion de un modelo evolutivo mediante la integracion temporal de elementos morfoestructurales y morfodinamicos.  1) la cartografia geomorfologica esta formada por un mapa morfotectonico y un mapa geomorfologico de detalle, ambos a escala 1:50.000.  2) la definicion de las unidades morfoestructurales se interpreta a partir del estudio de los fundamentos geologicos, tectonicos y la interpretacion geodinamica. Se realiza asimismo la formacion de un mapa geologico de sintesis y un mapa de fracturas.  3) la catalogacion de las formas del relieve: generadas por tectonica, asociadas al contexto estructural (formas graniticas), acciones fluviales y asociadas a dominios morfoclimaticos.  4) el modelo evolutivo registra una historia geomorfologica con diferentes etapas desde el paleozoico hasta nuestros dias. El bloque cristalino de avila se define como un conjunto de bloques tectonicos o dovelas articulados en torno a la falla cortical de plasencia.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Geomorfolog\u00eda del area de contacto del sistema central con la cuenca del duero entre los rios adaja y tormes<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Geomorfolog\u00eda del area de contacto del sistema central con la cuenca del duero entre los rios adaja y tormes <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Miguel Herrero Matias <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1993<\/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>Julio Mu\u00f1oz Jimenez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan Sanz Donaire <\/li>\n<li>Antonio Arozarena Villar (vocal)<\/li>\n<li>Eduardo Martinez De Pison Stampa (vocal)<\/li>\n<li>Concepcion Sanz Herraiz (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Miguel Herrero Matias El trabajo presenta el estudio geomorfologico del sector de zocalo (granitico) que se identifica [&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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