{"id":120899,"date":"2023-11-28T13:23:49","date_gmt":"2023-11-28T13:23:49","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-petrofisica-y-alterabilidad-de-calizas-y-dolomias\/"},"modified":"2023-11-28T13:23:49","modified_gmt":"2023-11-28T13:23:49","slug":"caracterizacion-petrofisica-y-alterabilidad-de-calizas-y-dolomias","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/caracterizacion-petrofisica-y-alterabilidad-de-calizas-y-dolomias\/","title":{"rendered":"Caracterizacion petrofisica y alterabilidad de calizas y dolomias"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Alonso Rodriguez Francisco Javier <\/strong><\/h2>\n<p>Se han estudiado de forma comparativa ocho variedades rocosas carbonatadas  desde rocas micriticas (c. Paramo c. Laspra) a cristalinas (c.Monta\u00f1a  d.Bo\u00f1ar); atendiendo a su petrografia  sistema poroso  propiedades fisicas y alterabilidad. El analisis del sistema poroso incluye la observacion directa de los poros  la determinacion de la porosidad y la distribucion de tama\u00f1os de poros (mediante tecnicas de inyeccion de mercurio). Se ha obtenido la cinetica de los procesos de sorcion de agua por las rocas para diferentes tipos de ensayos; asi como la velocidad de propagacion de ondas elasticas y la resistencia a la traccion indirecta. Se han revisado y llevado a cabo diferentes ensayos de alterabilidad  valorandose los da\u00f1os sobre las rocas  de la observacion de su superficie y de las variaciones en los parametros fisicos preestablecidos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracterizacion petrofisica y alterabilidad de calizas y dolomias<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracterizacion petrofisica y alterabilidad de calizas y dolomias <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Alonso Rodriguez Francisco Javier <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1986<\/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> Esbert Alemany Rosa M.<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Fernando Juan Ramos Galino <\/li>\n<li>Federico Orti Cabo (vocal)<\/li>\n<li> Montoto San Miguel Modesto (vocal)<\/li>\n<li>Carlos Oteo Mazo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Alonso Rodriguez Francisco Javier Se han estudiado de forma comparativa ocho variedades rocosas carbonatadas desde rocas micriticas [&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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