{"id":29250,"date":"2018-03-09T09:22:18","date_gmt":"2018-03-09T09:22:18","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-geomorfologico-y-reconstruccion-de-paleopaisajes-neogenos-y-cuaternarios-en-la-sierra-de-atapuerca-y-el-valle-medio-del-ra%c2%ado-arlanzon\/"},"modified":"2018-03-09T09:22:18","modified_gmt":"2018-03-09T09:22:18","slug":"analisis-geomorfologico-y-reconstruccion-de-paleopaisajes-neogenos-y-cuaternarios-en-la-sierra-de-atapuerca-y-el-valle-medio-del-ra%c2%ado-arlanzon","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-geomorfologico-y-reconstruccion-de-paleopaisajes-neogenos-y-cuaternarios-en-la-sierra-de-atapuerca-y-el-valle-medio-del-ra%c2%ado-arlanzon\/","title":{"rendered":"An\u00e1lisis geomorfol\u00f3gico y reconstrucci\u00f3n de paleopaisajes ne\u00f3genos y cuaternarios en la sierra de atapuerca y el valle medio del r\u00edo arlanz\u00f3n"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Alfonso Benito Calvo <\/strong><\/h2>\n<p>Se ha realizado el an\u00e1lisis geomorfol\u00f3gico del sector nororiental de la cuenca del duero, enfocado a definir geomorfol\u00f3gica en la sierra de atapuerca y el valle medio del r\u00edo arlanz\u00f3n, para relacionar la evoluci\u00f3n del relieve con el desarrollo del sistema endok\u00e1rsico de esta sierra donde se localizan los yacimientos arqueopaleontol\u00f3gicos pleistocenos. En el estudio geomorfol\u00f3gico se han tratado las principales unidades morfol\u00f3gicas de la regi\u00f3n, como son la superficies de erosi\u00f3n intraterciarias, las superficies polig\u00e9nicas de los p\u00e1ramos y sus implicaciones en la conexi\u00f3n duero-bureda, la descripci\u00f3n de las morfolog\u00edas exok\u00e1rsticas, y el an\u00e1lisis morfol\u00f3gico de los valles fluviales. Por medio de las cartograf\u00edas elaboradas (cartograf\u00edas geomorfol\u00f3gicas 1:10.000 y 1:25:000) y la construcci\u00f3n de un mde (10 metros de resoluci\u00f3n), se ha acometido la reconstrucci\u00f3n de los paleo-relieves ne\u00f3genos y cuaternarios a partir de la restituci\u00f3n estad\u00edstica de las morfolog\u00edas relictas o paleosuperficies, utilizando sig. Gracias a las reconstrucciones se han establecido nuevas relaciones de la evoluci\u00f3n geomorfol\u00f3gica con la formaci\u00f3n y desarrollo de los yaciemientos, y a su vez ha permitido elaborar un m\u00e9todo de an\u00e1lisis cuantitativo de paleopaisajes, basado en la clasificaci\u00f3n estad\u00edstica y litol\u00f3gica del territorio, que aplicado a los relieves reconstruidos ha permitido obtener la evoluci\u00f3n del mosaico del paisaje durante el ne\u00f3geno y el cuaternario. Este an\u00e1lisis evolutivo del paisaje se ha medido en funci\u00f3n de la variaci\u00f3n de las variables topogr\u00e1ficas, en funci\u00f3n de la evoluci\u00f3n espacial de las unidades f\u00edsicas del territorio y en funci\u00f3n de los \u00edndices m\u00e9tricos del paisaje de uso m\u00e1s frecuentes en ecolog\u00edas del paisaje, relacionando estos atributos del paisaje con la formaci\u00f3n de los yacimientos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>An\u00e1lisis geomorfol\u00f3gico y reconstrucci\u00f3n de paleopaisajes ne\u00f3genos y cuaternarios en la sierra de atapuerca y el valle medio del r\u00edo arlanz\u00f3n<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 An\u00e1lisis geomorfol\u00f3gico y reconstrucci\u00f3n de paleopaisajes ne\u00f3genos y cuaternarios en la sierra de atapuerca y el valle medio del r\u00edo arlanz\u00f3n <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Alfonso Benito Calvo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 18\/03\/2004<\/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>Alfredo Perez Gonzalez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Luis Arsuaga ferreras <\/li>\n<li>mateo Guti\u00e9rrez elorza (vocal)<\/li>\n<li>Antonio Cendrero uceda (vocal)<\/li>\n<li> Goy goy Jos\u00e9 Luis (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alfonso Benito Calvo Se ha realizado el an\u00e1lisis geomorfol\u00f3gico del sector nororiental de la cuenca del duero, [&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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