{"id":155036,"date":"2026-01-12T17:16:32","date_gmt":"2026-01-12T17:16:32","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/caracterizacion-de-la-respuesta-sismica-local-en-las-cuencas-de-granada-espana-y-ciudad-guzman-mexico-mediante-el-analisis-espectral-de-microtremores-y-terremotos\/"},"modified":"2026-01-12T17:16:32","modified_gmt":"2026-01-12T17:16:32","slug":"caracterizacion-de-la-respuesta-sismica-local-en-las-cuencas-de-granada-espana-y-ciudad-guzman-mexico-mediante-el-analisis-espectral-de-microtremores-y-terremotos","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/caracterizacion-de-la-respuesta-sismica-local-en-las-cuencas-de-granada-espana-y-ciudad-guzman-mexico-mediante-el-analisis-espectral-de-microtremores-y-terremotos\/","title":{"rendered":"Caracterizacion de la respuesta sismica local en las cuencas de granada (espa\u00f1a) y ciudad guzman (mexico) mediante el analisis espectral de microtremores y terremotos."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jos\u00e9 Morales Soto <\/strong><\/h2>\n<p>Se ha estudiado la estructura del basamento de la depresion de granada mediante datos gravimetricos y perfiles sismicos de reflexion. Se ha evaluado la respuesta sismica local en las cuencas de granada y zafarraya (espa\u00f1a) y ciudad guzman (mexico) mediante el analisis espectral de microtremores y microterremotos, realizandose un estudio en detalle de las frecuencias naturales en la ciudad de granada, mediante la elaboracion de un mapa de isoperiodos dominantes, como una contribucion a la microzonacion sismica.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Caracterizacion de la respuesta sismica local en las cuencas de granada (espa\u00f1a) y ciudad guzman (mexico) mediante el analisis espectral de microtremores y terremotos.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Caracterizacion de la respuesta sismica local en las cuencas de granada (espa\u00f1a) y ciudad guzman (mexico) mediante el analisis espectral de microtremores y terremotos. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jos\u00e9 Morales Soto <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/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>Francisco De Asis Vidal Sanchez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Jos\u00e9 Antonio Canas Torres <\/li>\n<li> Miguel Martinez Fernando De (vocal)<\/li>\n<li>Miguel Herraiz Sarachaga (vocal)<\/li>\n<li>Jos\u00e9 Rodriguez Fernandez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jos\u00e9 Morales Soto Se ha estudiado la estructura del basamento de la depresion de granada mediante datos [&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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