{"id":77421,"date":"2018-03-09T23:22:57","date_gmt":"2018-03-09T23:22:57","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/inestabilidades-submarinas-caracterizacion-sedimentaria-y-factores-de-control\/"},"modified":"2018-03-09T23:22:57","modified_gmt":"2018-03-09T23:22:57","slug":"inestabilidades-submarinas-caracterizacion-sedimentaria-y-factores-de-control","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/barcelona\/inestabilidades-submarinas-caracterizacion-sedimentaria-y-factores-de-control\/","title":{"rendered":"Inestabilidades submarinas: caracterizaci\u00f3n sedimentaria y factores de control"},"content":{"rendered":"<h2>Tesis doctoral de <strong> David Casas Layola <\/strong><\/h2>\n<p>Esta tesis doctoral es una contribuci\u00f3n al conocimiento de las inestabilidades submarinas en diferentes contextos geol\u00f3gicos y con diferentes grados de resoluci\u00f3n, resultado de la aplicaci\u00f3n de diferentes t\u00e9cnicas de estudio. La memoria adem\u00e1s est\u00e1 concebida como una integraci\u00f3n de art\u00edculos en revistas cient\u00edficas incluidas en el science citation index.     el estudio de las inestabilidades sedimentarias submarinas se han estructurado en el desarrollo de cuatro objetivos b\u00e1sicos que forman seg\u00fan la hip\u00f3tesis de la tesis el esqueleto b\u00e1sico para el conocimiento de estos procesos y la caracterizaci\u00f3n del riesgo geol\u00f3gico asociado a ellos:     1,- caracterizaci\u00f3n del margen continental y registro hist\u00f3rico de las inestabilidades submarinas.     2,- definici\u00f3n de facies sedimentarias, geometr\u00eda, din\u00e1mica de rotura y evoluci\u00f3n de los deslizamientos.     3,- estudio de las propiedades f\u00edsicas, mec\u00e1nicas y el\u00e1sticas del sedimento.     4,- determinaci\u00f3n de las fuerzas y procesos mec\u00e1nicos que pueden controlar la detonaci\u00f3n de deslizamientos.     las inestabilidades submarinas son un importante mecanismos modelador de m\u00e1rgenes continentales, y en especial del talud continental. para la caracterizaci\u00f3n del riesgo geol\u00f3gico es esencial tener en cuenta todos los factores cr\u00edticos que permiten realizar un an\u00e1lisis detallado del terreno como son: la localizaci\u00f3n y distribuci\u00f3n de las inestabilidades, par\u00e1metros fisiogr\u00e1ficos, localizaci\u00f3n de los sistemas sedimentarios, morfolog\u00eda y configuraci\u00f3n interna de las inestabilidades, facies litol\u00f3gicas y ac\u00fasticas, elementos morfo-sedimentarios y morfo-estructurales y finalmente la din\u00e1mica de fluidos.     la caracterizaci\u00f3n del riesgo geol\u00f3gico requiere adem\u00e1s aproximaciones pluridisciplinares que combinen \u00abmodelos ac\u00fasticos\u00bb con \u00abmodelos geot\u00e9cnicos\u00bb detallados que puedan explicar toda la variabilidad gen\u00e9tica y morfol\u00f3gica de las inestabilidades de un margen.     las<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Inestabilidades submarinas: caracterizaci\u00f3n sedimentaria y factores de control<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Inestabilidades submarinas: caracterizaci\u00f3n sedimentaria y factores de control <\/li>\n<li><strong>Autor:<\/strong>\u00a0 David Casas Layola <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 28\/11\/2005<\/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>Gemma Ercilla<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: federico Vilas <\/li>\n<li>eul\u00ed\u00a0lia Gr\u00ed\u00a0cia (vocal)<\/li>\n<li>Luis Somoza losada (vocal)<\/li>\n<li>francesco Chiocci (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de David Casas Layola Esta tesis doctoral es una contribuci\u00f3n al conocimiento de las inestabilidades submarinas en diferentes [&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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