{"id":134213,"date":"1997-01-01T00:00:00","date_gmt":"1997-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/los-sistemas-karsticos-de-la-provincia-de-malaga-y-su-evolucion-contribucion-al-conocimiento-paleoclimatico-del-cuaternario-en-el-mediterraneo-occidental\/"},"modified":"1997-01-01T00:00:00","modified_gmt":"1997-01-01T00:00:00","slug":"los-sistemas-karsticos-de-la-provincia-de-malaga-y-su-evolucion-contribucion-al-conocimiento-paleoclimatico-del-cuaternario-en-el-mediterraneo-occidental","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/los-sistemas-karsticos-de-la-provincia-de-malaga-y-su-evolucion-contribucion-al-conocimiento-paleoclimatico-del-cuaternario-en-el-mediterraneo-occidental\/","title":{"rendered":"Los sistemas karsticos de la provincia de malaga y su evolucion: contribucion al conocimiento paleoclimatico del cuaternario en el mediterraneo occidental."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Juan  Jos\u00e9 Dur\u00e1n Valsero <\/strong><\/h2>\n<p>Los sistemas karsticos de la provincia de malaga ocupan una sexta parte de su superficie. La karstificacion se desarrolla preferentemente en los materiales carbonatados mesozoicos del penibetico y de la dorsal betica. Existen evidencias en el conjunto de macizos karsticos de una dilatada evolucion, que arranca del mioceno superior, bajo condiciones climaticas cambiantes en el tiempo. El estudio de los diferentes depositos sedimentarios ligados al endo y al exokarst (espeleotemas, sedimentos detriticos y travertinos), ha permitido establecer la existencia de periodos, durante el cuaternario, favorables a la genesis de carbonatos continentales.  estos periodos, acotados mediante tecnicas de datacion absoluta (esr y th\/u), se correlacionan claramente con los estadios isotopicos calidos de la curva de variaciones del 180 en los sedimentos oceanicos profundos (11, 9, 7, 5, 3 y 1). Las paleotemperaturas estimadas para estos periodos son semejantes a las actuales, con variaciones del mismo orden de magnitud que las derivadas del gradiente altitudinal actual. Es posible que la deposicion de importantes volumenes de carbonatos en fases calidas actue como mecanismo regulador del clima (sumidero de co2).<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Los sistemas karsticos de la provincia de malaga y su evolucion: contribucion al conocimiento paleoclimatico del cuaternario en el mediterraneo occidental.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Los sistemas karsticos de la provincia de malaga y su evolucion: contribucion al conocimiento paleoclimatico del cuaternario en el mediterraneo occidental. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Juan  Jos\u00e9 Dur\u00e1n Valsero <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1997<\/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>Jeronimo Lopez Martinez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Pedraza Gilsanz JavierDe <\/li>\n<li>Francisco Carrasco Cantos (vocal)<\/li>\n<li>Rene Lhenaff (vocal)<\/li>\n<li>Emilio Reyes Camacho (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Juan Jos\u00e9 Dur\u00e1n Valsero Los sistemas karsticos de la provincia de malaga ocupan una sexta parte 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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