{"id":42976,"date":"2018-03-16T07:19:40","date_gmt":"2018-03-16T07:19:40","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/contribucion-al-conocimiento-geomorfologico-de-la-depresion-central-catalana\/"},"modified":"2018-03-16T07:19:40","modified_gmt":"2018-03-16T07:19:40","slug":"contribucion-al-conocimiento-geomorfologico-de-la-depresion-central-catalana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/contribucion-al-conocimiento-geomorfologico-de-la-depresion-central-catalana\/","title":{"rendered":"Contribucion al conocimiento geomorfologico de la depresion central catalana."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jaime Calvet Porta <\/strong><\/h2>\n<p>Se efectua el estudio geomorfologico de seis sectores representativos  en los que coexisten los procesos de incision y acumulacion. Todo ello se acompa\u00f1a de mapas y esquemas geomorfologicos. Se pone en evidencia la falta de datos que permitan asegurar la accion de procesos priglaciares  durante el cuaternario  en los sectores estudiados. Se pone de manifiesto la gran importancia de los procesos de escurrimiento difuso que han modelado un relieve eminentemente estructural. Se estudian a su vez algunas formas debidas a la neotectonica cuaternaria.  como conclusiones generales se observa la transicion de e a w  desde sistemas morfogeneticas subhumedas a semiaridos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Contribucion al conocimiento geomorfologico de la depresion central catalana.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Contribucion al conocimiento geomorfologico de la depresion central catalana. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jaime Calvet Porta <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1977<\/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>Luis Sole Sabaris<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Luis Sole Sabaris <\/li>\n<li>Salvador Llobet Reverter (vocal)<\/li>\n<li>Oriol Riba Arderiu (vocal)<\/li>\n<li>Jean Tricart Jean (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jaime Calvet Porta Se efectua el estudio geomorfologico de seis sectores representativos en los que coexisten los [&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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