{"id":51944,"date":"2021-12-11T05:54:54","date_gmt":"2021-12-11T05:54:54","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/geomorfologia-de-las-sierras-exteriores-oscenses-y-su-piedemonte\/"},"modified":"2021-12-11T05:54:54","modified_gmt":"2021-12-11T05:54:54","slug":"geomorfologia-de-las-sierras-exteriores-oscenses-y-su-piedemonte","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geomorfologia-de-las-sierras-exteriores-oscenses-y-su-piedemonte\/","title":{"rendered":"Geomorfolog\u00eda de las sierras exteriores oscenses y su piedemonte"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Joaquin Rodriguez Vidal <\/strong><\/h2>\n<p>Se realiza un estudio geomorfologico del sector central de las sierras exteriores oscenses y su piedemonte con un cartografia a escala 1:50.000; diferenciandose tres superficies de erosion en las sierras que se datan aproximadamente como oligoreno superior  intramioceno y pliocuaternario  con una importante fase de deformacion de edad mioceno superior. En la zona de piedemonte se diferencian tres niveles de acumulacion pliocuaternaria con morfolog\u00eda de abanicos aluviales  encajados unos en otros y que superen el inicio de la red fluvial cuaternaria  cuya evidencia morfologica se representa por medio de cinco niveles de terrazas que evolucionan espacial y temporalmente a lo largo del sementano oscense. Por ultimo se analizan los procesos morfogeneticos actuales de base a la distribucion morfoclimatica  evidenciandose la actuacion de los sistemas periglaciar  templado humedo y semidrido.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Geomorfolog\u00eda de las sierras exteriores oscenses y su piedemonte<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Geomorfolog\u00eda de las sierras exteriores oscenses y su piedemonte <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Joaquin Rodriguez Vidal <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1983<\/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>Mateo Guti\u00e9rrez Elorza<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Vicente Sanchez Cela <\/li>\n<li>Leandro Sequeiros Sanroman (vocal)<\/li>\n<li>Mateo Guti\u00e9rrez Elorza (vocal)<\/li>\n<li>Francisco Alberto Gimenez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Joaquin Rodriguez Vidal Se realiza un estudio geomorfologico del sector central de las sierras exteriores oscenses y [&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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