{"id":155099,"date":"2026-01-12T17:17:00","date_gmt":"2026-01-12T17:17:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-y-sedimentologia-del-relleno-aluvial-de-la-cuenca-de-guadix-cordilleras-beticas\/"},"modified":"2026-01-12T17:17:00","modified_gmt":"2026-01-12T17:17:00","slug":"estratigrafia-y-sedimentologia-del-relleno-aluvial-de-la-cuenca-de-guadix-cordilleras-beticas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-y-sedimentologia-del-relleno-aluvial-de-la-cuenca-de-guadix-cordilleras-beticas\/","title":{"rendered":"Estratigrafia y sedimentolog\u00eda del relleno aluvial de la cuenca de guadix (cordilleras beticas)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Cesar Viseras Alarcon <\/strong><\/h2>\n<p>La cuenca continental de guadix se estructura hacia el ventiense y en su relleno se pueden diferenciar tres unidades de caracter tectosedimentario (utss), la uts inferior corresponde a la fm. Rio gor y supone la respuesta a la estructuracion tectonica que condiciona la brusca retirada del mar de la cuenca tortoniense. Los depositos mas caracteristicos corresponden a un sistema de conos de deyeccion de escasa progradacion hacia el centro de cuenca. Las utss intermedia y superior (aproximadamente rusciniense y villafranquiense-pleistoceno, respectivamente) corresponden a las fm. Guadix y gorafe-huelago de origen aluvial y lacustre, que cambian de facies entre si. Para ellas se deduce un esquema de arquitectura estratigrafica consistente en la existencia de dos sistemas de abanicos aluviales transversales y un sistema fluvial longitudinal de caracter meandriforme, que transcurre por el sector axial de la cuenca, coincidiendo en parte con las areas de sedimentacion lacustre. A lo largo de toda la historia de la cuenca se detecta un continuo desplazamiento del eje hacia el margen subbetico (septentrional), como consecuencia de un progresivo aumento en la relacion aportes\/subsidencia en el margen betico (meridional).  este proceso se acentua en la tercera unidad por causa de la mayor actividad climatica en los relieves de sierra nevada y sierra de baza.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia y sedimentolog\u00eda del relleno aluvial de la cuenca de guadix (cordilleras beticas).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia y sedimentolog\u00eda del relleno aluvial de la cuenca de guadix (cordilleras beticas). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Cesar Viseras Alarcon <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/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>Juan Fernandez Martinez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Juan  Antonio Vera Torres <\/li>\n<li>Mar\u00eda no Marzo Carpio (vocal)<\/li>\n<li>John Bluck Brian (vocal)<\/li>\n<li>Pedro Alejandro Ru\u00edz Ort\u00edz (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Cesar Viseras Alarcon La cuenca continental de guadix se estructura hacia el ventiense y en su relleno [&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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