{"id":155176,"date":"2026-01-12T17:17:37","date_gmt":"2026-01-12T17:17:37","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-de-los-litosomas-del-cretacico-mediante-diagrafias-y-otras-tecnicas-del-subsuelo\/"},"modified":"2026-01-12T17:17:37","modified_gmt":"2026-01-12T17:17:37","slug":"caracterizacion-de-los-litosomas-del-cretacico-mediante-diagrafias-y-otras-tecnicas-del-subsuelo","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/caracterizacion-de-los-litosomas-del-cretacico-mediante-diagrafias-y-otras-tecnicas-del-subsuelo\/","title":{"rendered":"Caracterizacion de los litosomas del cretacico mediante diagrafias y otras tecnicas del subsuelo."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Enrique Aracil Avila <\/strong><\/h2>\n<p>Esta tesis doctoral es un trabajo metodologico en el que se han empleado las tecnicas propias de la geolog\u00eda del subsuelo, aplicandolas a los materiales del cretacico.  dentro de estas tecnicas se han empleado: estudio de diagrafias, con el que se han logrado caracterizar las diferentes unidades litoestratigraficas del cretacico, pudiendose determinar las propiedades que muestran en estas curvas las diferentes unidades. Con los sondeos hidrogeologicos se han realizado interpretaciones de la geometria de algunas cuencas, como en los llanos de albacete, asi como tectonicas, con la creacion de un modelo del diapirismo en el area de jumilla-villena (murcia). Con los mapas aeromagneticos se han propuesto unos dominios a escala regional basandose en el caracter de las anomalias. Por ultimo, con las lineas sismicas se han determinado los fenomenos halocineticos y diapiricos que afectan a la zona de leda\u00f1a (albacete) y se han levantado mapas de isobatas del cretacico inferior en la zona de calasparra (murcia).<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracterizacion de los litosomas del cretacico mediante diagrafias y otras tecnicas del subsuelo.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracterizacion de los litosomas del cretacico mediante diagrafias y otras tecnicas del subsuelo. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Enrique Aracil Avila <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/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>Lorenzo Vilas Minondo<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Alvaro Garcia Quintana <\/li>\n<li>Rudolf Merten (vocal)<\/li>\n<li>Ramon Querol Muller (vocal)<\/li>\n<li>Jos\u00e9 Ramirez Del Pozo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Enrique Aracil Avila Esta tesis doctoral es un trabajo metodologico en el que se han empleado las [&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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