{"id":15381,"date":"2002-01-02T00:00:00","date_gmt":"2002-01-02T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/reconstruccion-paleoambiental-de-la-depresion-de-granada-a-traves-del-estudio-de-paleosuelos\/"},"modified":"2002-01-02T00:00:00","modified_gmt":"2002-01-02T00:00:00","slug":"reconstruccion-paleoambiental-de-la-depresion-de-granada-a-traves-del-estudio-de-paleosuelos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/reconstruccion-paleoambiental-de-la-depresion-de-granada-a-traves-del-estudio-de-paleosuelos\/","title":{"rendered":"Reconstrucci\u00f3n paleoambiental de la depresi\u00f3n de granada a trav\u00e9s del estudio de paleosuelos"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Irene Ortiz Bernad <\/strong><\/h2>\n<p>Al igual que los dep\u00f3sitos estratigr\u00e1ficos son utilizados para la reconstrucci\u00f3n paleogeogr\u00e1fica de los episodios morfogen\u00e9ticos o erosivos, el estudio de paleosuelos puede ser empleado para la reconstrucciones paleoambientales de los episodios edafogen\u00e9ticos o de estabilidad.  en este trabajo se estudian las caracter\u00edsticas de una serie de paleosuelos desarrollados sobre distintas superficies geomorfol\u00f3gicas de la depresi\u00f3n de granada y sierra nevada (se espa\u00f1a) desde el plioceno que, por sus especiales rasgos topogr\u00e1ficos han permitido la conservaci\u00f3n de estos suelos. Los resultados del estudio realizado han servido para interpretar los procesos que dieron lugar a la formaci\u00f3n de estos suelos e inferir las condiciones ambientales reinantes durante su edafog\u00e9nesis, as\u00ed como establecer la evoluci\u00f3n paleoambiental de la depresi\u00f3n de granada desde finales del mioceno hasta nuestros d\u00edas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Reconstrucci\u00f3n paleoambiental de la depresi\u00f3n de granada a trav\u00e9s del estudio de paleosuelos<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Reconstrucci\u00f3n paleoambiental de la depresi\u00f3n de granada a trav\u00e9s del estudio de paleosuelos <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Irene Ortiz Bernad <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/02\/2002<\/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>Mar\u00eda no Simon Torres<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: jos\u00e9 Aguilar ru\u00edz <\/li>\n<li> Calvo de anta rosa (vocal)<\/li>\n<li>george Stoops (vocal)<\/li>\n<li>Rafael Espejo serrano (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Irene Ortiz Bernad Al igual que los dep\u00f3sitos estratigr\u00e1ficos son utilizados para la reconstrucci\u00f3n paleogeogr\u00e1fica de 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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