{"id":156181,"date":"2026-01-12T17:26:54","date_gmt":"2026-01-12T17:26:54","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-plio-pleistoceno-de-la-cuenca-de-guadix-baza-zona-occidental-y-area-de-cullar-baza-estratigrafia-sedimentologia-tafonomia-y-yacimientos-de-vertebrados\/"},"modified":"2026-01-12T17:26:54","modified_gmt":"2026-01-12T17:26:54","slug":"el-plio-pleistoceno-de-la-cuenca-de-guadix-baza-zona-occidental-y-area-de-cullar-baza-estratigrafia-sedimentologia-tafonomia-y-yacimientos-de-vertebrados","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-plio-pleistoceno-de-la-cuenca-de-guadix-baza-zona-occidental-y-area-de-cullar-baza-estratigrafia-sedimentologia-tafonomia-y-yacimientos-de-vertebrados\/","title":{"rendered":"El plio-pleistoceno de la cuenca de guadix-baza (zona occidental y area de cullar-baza): estratigrafia, sedimentolog\u00eda, tafonomia y yacimientos de vertebrados."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Alonso Diago M. Angeles <\/strong><\/h2>\n<p>Los materiales sedimentarios continentales, neogenos y cuaternarios que rellenan la zona occidental de la depresion de guadix-baza quedan divididos en tres unidades estratigraficas: unidad inferior, unidad superior y unidad de abanicos aluviales y glacis terminales. Desde el punto de vista sedimentologico en las unidades inferior y superior se reconocen ambientes deposicionales aluviales (abanicos aluviales con facies proximales y medias) y fluviales (rios trenzados), en el borde n del area, muy proximos al sustrato subbetico se desarrollaron dos areas lacustres carbonatadas de aguas dulces en diferentes lapsos de tiempo. En el area de cullar-baza se definen 4 unidades estratigraficas: tramo de arenas y conglomerados rojos tramo de arenas amarillas, tramo de dolomias y yesos y tramo carbonatado superior. Se estudia la tafonomia y ambiente sedimentario de los yacimientos de vertebrados de huelago, huescar y cullar-baza. El primero es un yacimiento \u00abin situ\u00bb parcialmente removilizado por corrientes, el segundo es transportado y el tercero esta \u00abin situ\u00bb en una zona palustre.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El plio-pleistoceno de la cuenca de guadix-baza (zona occidental y area de cullar-baza): estratigrafia, sedimentolog\u00eda, tafonomia y yacimientos de vertebrados.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El plio-pleistoceno de la cuenca de guadix-baza (zona occidental y area de cullar-baza): estratigrafia, sedimentolog\u00eda, tafonomia y yacimientos de vertebrados. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Alonso Diago M. Angeles <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1991<\/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>Manuel Hoyos Gomez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jes\u00fas (secretario) Carballeira Cueto <\/li>\n<li>Caridad Zazo Carde\u00f1a (vocal)<\/li>\n<li>Mar\u00eda  Teresa Alberdi Alonso (vocal)<\/li>\n<li>  (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alonso Diago M. Angeles Los materiales sedimentarios continentales, neogenos y cuaternarios que rellenan la zona occidental de [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,245,953,9386,3857],"tags":[270284,18979,270285,7598,27338],"class_list":["post-156181","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-estratigrafia","category-geologia","category-salamanca","category-sedimentologia","tag-alonso-diago-m-angeles","tag-caridad-zazo-cardena","tag-jesus-secretario-carballeira-cueto","tag-manuel-hoyos-gomez","tag-maria-teresa-alberdi-alonso"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/156181","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=156181"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/156181\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=156181"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=156181"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=156181"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}