{"id":36380,"date":"1998-01-01T00:00:00","date_gmt":"1998-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/magnetoestratigrafia-i-litoestratigrafia-a-la-conca-de-guadix-baza-i-altres-punts-del-neogen-continental-de-les-serralades-betiques\/"},"modified":"1998-01-01T00:00:00","modified_gmt":"1998-01-01T00:00:00","slug":"magnetoestratigrafia-i-litoestratigrafia-a-la-conca-de-guadix-baza-i-altres-punts-del-neogen-continental-de-les-serralades-betiques","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/magnetoestratigrafia-i-litoestratigrafia-a-la-conca-de-guadix-baza-i-altres-punts-del-neogen-continental-de-les-serralades-betiques\/","title":{"rendered":"Magnetoestratigrafia i litoestratigrafia a la conca de guadix-baza i altres punts del neogen continental de les serralades betiques."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Oriol Oms Llobet <\/strong><\/h2>\n<p>Se ha estudiado la magnetoestratigraf\u00eda de varias secciones continentales plio-pleistocenas en cuencas neogenas de las cordilleras b\u00e9ticas (granada, jerez y, principalmente, guadix-baza). La correlaci\u00f3n de las polaridades obtenidas con la escala temporal de la polaridad geomagn\u00e9tica permite una correlaci\u00f3n de la escala cronoestratigr\u00e1fica continental con la escala estandard (marina) para todo el plio-pleistoceno.  a la vez, los estudios litoestratigr\u00e1ficos realizados en guadix-baza permite la evidencia f\u00edsica de sucesi\u00f3n de yacimientos (validando as\u00ed los criterios basados en la paleontolog\u00eda). Tambi\u00e9n se obtiene un modelo de cambio clim\u00e1tico para el plioceno basado en el an\u00e1lisis cicloestratigr\u00e1fico, dotado de las dataciones absolutas que suponen los cambios de polaridad.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Magnetoestratigrafia i litoestratigrafia a la conca de guadix-baza i altres punts del neogen continental de les serralades betiques.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Magnetoestratigrafia i litoestratigrafia a la conca de guadix-baza i altres punts del neogen continental de les serralades betiques. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Oriol Oms Llobet <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Aut\u00f3noma de barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1998<\/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>Jordi Agusti Ballester<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Vicente Soler Javaloyes <\/li>\n<li>Gloria Cuenca Besc\u00f3s (vocal)<\/li>\n<li>Pedro Anadon Monzon (vocal)<\/li>\n<li>Cesar Viseras Alarcon (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Oriol Oms Llobet Se ha estudiado la magnetoestratigraf\u00eda de varias secciones continentales plio-pleistocenas en cuencas neogenas 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 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