{"id":48636,"date":"2020-11-08T01:33:24","date_gmt":"2020-11-08T01:33:24","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-sistema-iberico-zaragozano-los-macizos-paleozoicos-y-su-entorno-estudio-geomorfologico\/"},"modified":"2020-11-08T01:33:24","modified_gmt":"2020-11-08T01:33:24","slug":"el-sistema-iberico-zaragozano-los-macizos-paleozoicos-y-su-entorno-estudio-geomorfologico","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-sistema-iberico-zaragozano-los-macizos-paleozoicos-y-su-entorno-estudio-geomorfologico\/","title":{"rendered":"El sistema iberico zaragozano: los macizos paleozoicos y su entorno. estudio geomorfologico."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Yetano Ruiz Luis Miguel <\/strong><\/h2>\n<p>El presente trabajo representa un estudio de los macizos paleozoicos zaragozanos desde el punto de vista de su evolucion geomorfologica  haciendo incapie en la evolucion posterior a la orogemia alpina  y por tanto al modelado que se ha realizado durante el cuaternario y que representa el paisaje que actualmente contemplamos. Como hipotesis se parte de que la superficie de erosion fini-terciaria condiciona toda la evolucion posterior del relieve al permitir la instalacion de la red fluvial en sus direcciones actuales; red fluvial que va a dirigir una erosion diferencial que rejuvenecera el relieve. El estudio de los depositos cuaternarios contribuye a conocer las crisis climaticas cuaternarias y a establecer una cronolog\u00eda relativa en esa evolucion.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El sistema iberico zaragozano: los macizos paleozoicos y su entorno. estudio geomorfologico.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El sistema iberico zaragozano: los macizos paleozoicos y su entorno. estudio geomorfologico. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Yetano Ruiz Luis Miguel <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/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>Salvador Mensua Fernandez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Salvador Mensua Fernandez <\/li>\n<li>Antonio Higueras Arnal (vocal)<\/li>\n<li>Alfredo Pablo Florist\u00e1n Im\u00edzcoz (vocal)<\/li>\n<li>Francisco Javier Martinez Gil (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Yetano Ruiz Luis Miguel El presente trabajo representa un estudio de los macizos paleozoicos zaragozanos desde el [&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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