{"id":139065,"date":"2026-01-12T17:40:54","date_gmt":"2026-01-12T17:40:54","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/tecnicas-geodesicas-y-geodinamicas-aplicadas-a-la-investigacion-del-riesgo-volcanico-en-la-isla-de-lanzarote\/"},"modified":"2026-01-12T17:40:54","modified_gmt":"2026-01-12T17:40:54","slug":"tecnicas-geodesicas-y-geodinamicas-aplicadas-a-la-investigacion-del-riesgo-volcanico-en-la-isla-de-lanzarote","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/tecnicas-geodesicas-y-geodinamicas-aplicadas-a-la-investigacion-del-riesgo-volcanico-en-la-isla-de-lanzarote\/","title":{"rendered":"\u00abtecnicas geodesicas y geodinamicas aplicadas a la investigacion del riesgo volcanico en la isla de lanzarote\u00bb."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jose Fernandez Torres <\/strong><\/h2>\n<p>Se resuelven teoricamente las ecuaciones de navier-stokes en un medio elastico estratificado, con dos capas y un semiespacio, considerando la existencia de campo gravitatorio, suponiendo como fuente de perturbacion una masa puntual mas un centro de expansion que podrian representar una intrusion magmatica esferica en la corteza. La solucion exacta del sistema de ecuaciones en derivadas parciales se obtiene de una forma directamente programable utilizando la tecnica de matrices propagantes. De esta manera, y conocidas las caracteristicas de una corteza particular, se obtienen como soluciones las deformaciones verticales y variaciones de gravedad en la superficie del medio como haces de curvas en funcion de la distancia y profundidad de la intrusion.  esta modelizacion se ha aplicado al modelo cortical de la isla de lanzarote, definido por sismica en dos capas sobre el manto. Se ha parametrizado este modelo asignando las constantes de cada capa.  como resultado se ha determinado cuales son las tecnicas geodesicas aplicables en cada uno de los estados correspondientes a una posible intrusion en la isla y su posible evolucion en una crisis eruptiva.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>\u00abtecnicas geodesicas y geodinamicas aplicadas a la investigacion del riesgo volcanico en la isla de lanzarote\u00bb.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 \u00abtecnicas geodesicas y geodinamicas aplicadas a la investigacion del riesgo volcanico en la isla de lanzarote\u00bb. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jose Fernandez Torres <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1992<\/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>Ricardo Vieira D\u00edaz<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Agust\u00edn Ud\u00edas Vallina <\/li>\n<li>Enrique Alarcon Alvarez (vocal)<\/li>\n<li> Sevilla De Lerma Miguel (vocal)<\/li>\n<li> Diez Gil Jos\u00e9 L. (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jose Fernandez Torres Se resuelven teoricamente las ecuaciones de navier-stokes en un medio elastico estratificado, con dos [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,986,2265,953,42367],"tags":[5017,253563,5018,82583,36217,7620],"class_list":["post-139065","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-complutense-de-madrid","category-geodesia","category-geologia","category-vulcanologia","tag-agustin-udias-vallina","tag-diez-gil-jose-l","tag-enrique-alarcon-alvarez","tag-jose-fernandez-torres","tag-ricardo-vieira-diaz","tag-sevilla-de-lerma-miguel"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139065","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=139065"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/139065\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=139065"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=139065"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=139065"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}