{"id":1237,"date":"1994-01-01T00:00:00","date_gmt":"1994-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1994\/01\/01\/modelizacion-de-fases-sismicas-regionales\/"},"modified":"1994-01-01T00:00:00","modified_gmt":"1994-01-01T00:00:00","slug":"modelizacion-de-fases-sismicas-regionales","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/modelizacion-de-fases-sismicas-regionales\/","title":{"rendered":"Modelizacion de fases sismicas regionales"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Emilio Carre\u00f1o Herrero <\/strong><\/h2>\n<p>Se analizan en este trabajo las caracteristicas mas significativas de las fases sismicas especialmente en la fase lg. A continuacion se describen las principales lineas del metodo de sumatorio de numeros de onda que se ha utilizado para la generacion de sismogramas sinteticos. Despues, mediante modelizacion se estudia la influencia del modelo de mecanismo, funcion fuente, profundidad y cambio de estructura en las formas de onda.  se determinan a continuacion valores de atenuacion cortical para la peninsula a partir de la fase lg, obteniendose una division por zonas de igual valor del factor de calidad, asi como estructuras y funciones fuente a aplicar en la generacion de simogramas sinteticos y compararlos posteriormente con registros observados en diferentes estaciones. Se obtienen de esta forma precisiones en la determinacion del mecanismo focal y se resaltan especialmente los efectos de sitio en algunas estaciones.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Modelizacion de fases sismicas regionales<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Modelizacion de fases sismicas regionales <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Emilio Carre\u00f1o Herrero <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1994<\/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>Julio Mezcua Rodr\u00edguez<\/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>Antoni Roca Adrover (vocal)<\/li>\n<li>Antonio  Jes\u00fas Martin Martin (vocal)<\/li>\n<li>Enrique Alarcon Alvarez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Emilio Carre\u00f1o Herrero Se analizan en este trabajo las caracteristicas mas significativas de las fases sismicas especialmente [&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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