{"id":128763,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/secuencias-de-deposito-y-estructuracion-diapirica-en-mesozoico-y-neogeno-del-prebetico-y-golfo-de-valencia-desde-sondeos-y-lineas-sismicas\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"secuencias-de-deposito-y-estructuracion-diapirica-en-mesozoico-y-neogeno-del-prebetico-y-golfo-de-valencia-desde-sondeos-y-lineas-sismicas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/secuencias-de-deposito-y-estructuracion-diapirica-en-mesozoico-y-neogeno-del-prebetico-y-golfo-de-valencia-desde-sondeos-y-lineas-sismicas\/","title":{"rendered":"Secuencias de deposito y estructuracion diapirica en mesozoico y neogeno del prebetico y golfo de Valencia desde sondeos y lineas sismicas."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Martinez Del Olmo Wenceslao <\/strong><\/h2>\n<p>Los datos lito y bioestratigraficos, y las diagrafias de pozo que recogen los sondeos de hidrocarburos, permiten un tratamiento metodologico para su uso en el analisis estratigrafico secuencial; metodolog\u00eda que aplicada al mesozoico y cenozoico del golfo de Valencia, prebetico e iberico (43 sondeos) ha conducido a la caracterizacion de 55 secuencias de deposito y 130 cortejos sedimentarios, que conforman el primer esqueleto secuencial de la plataforma beti-iberica, y permiten interpretar sus diferentes fases de progradacion, retrogradacion y erosion. Esta interpretacion, llevada al neogeno del mediterraneo, como ejemplo, posibilita invalidar el modelo de desecacion propuesto para el messimiense. De otras parte, a traves de lineas sismicas y mapas de superficie, se llega a la diferenciacion de numerosas formas estructurales de origen diapirico que, creadas durante una larga etapa sedimentaria, han condicionado la inversion tectonica miocena y dificultan su interpretacion. Por ultimo, el registro estratigrafico secuencial es utilizado para diferenciar causas tectonicas, eustaticas, climaticas, topograficas, etc., Y en funcion de las cantidades de progradacion y localizacion de areas de sedimentacion, se establecen ocho geometrias de las secuencias de deposito individuales.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Secuencias de deposito y estructuracion diapirica en mesozoico y neogeno del prebetico y golfo de Valencia desde sondeos y lineas sismicas.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Secuencias de deposito y estructuracion diapirica en mesozoico y neogeno del prebetico y golfo de Valencia desde sondeos y lineas sismicas. <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Martinez Del Olmo Wenceslao <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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> Gomez Fernandez Juan  Jose<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carmina Virgili Rodon <\/li>\n<li>Juan  Antonio Vera Torres (vocal)<\/li>\n<li>Juan Rosell Sanuy (vocal)<\/li>\n<li>Alberto Garrido Megias (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Martinez Del Olmo Wenceslao Los datos lito y bioestratigraficos, y las diagrafias de pozo que recogen los [&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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