{"id":38139,"date":"2018-03-09T09:37:34","date_gmt":"2018-03-09T09:37:34","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/parametros-de-fuente-de-los-terremotos-del-mar-de-alboran\/"},"modified":"2018-03-09T09:37:34","modified_gmt":"2018-03-09T09:37:34","slug":"parametros-de-fuente-de-los-terremotos-del-mar-de-alboran","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/parametros-de-fuente-de-los-terremotos-del-mar-de-alboran\/","title":{"rendered":"Parametros de fuente de los terremotos del mar de alboran."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Taoufik Mourabit <\/strong><\/h2>\n<p>Se han analizado terremotos y microterremotos ocurridos en el mar de albor\u00e1n y zonas lim\u00edtrofes en el per\u00edodo 1994-97 para determinar su momento s\u00edsmico escalar, ca\u00edda de esfuerzos est\u00e1tica, energ\u00eda s\u00edsmica y tama\u00f1o de la fuente, as\u00ed como relaciones de escala entre estos par\u00e1metros. La zona de estudio se ha dividido entre varias regiones diferenciadas por razones sismotect\u00f3nicas. Alhucemas, roquetas de mar, motril, m\u00e1laga &#8211; superficiales y m\u00e1laga-intermedios y se han estudiado las diferencias significativas en la relajaci\u00f3n de esfuerzos entre ellas.  la metodolog\u00eda seguida ha consistido en el an\u00e1lisis espectral de fases p y s registradas en las estaciones s\u00edsmicas del instituto andaluz de geof\u00edsica. Una vez corregidos dichos espectros de respuesta instrumental, atenuaci\u00f3n de camino, superficie libre, radiaci\u00f3n y atenuaci\u00f3n local, para estimar el espectro de la fuente en campo lejano, se determinando por los m\u00e9todos de andrews y de snoke los par\u00e1metros espectrales omega0 (nivel de baja frecuencia) y fe (frecuencia esquina), asumiendo un modelo de brune. A partir de estos par\u00e1metros se han determinado los de fuente.  los valores de ca\u00edda de esfuerzos est\u00e1ticos obtenidos son en su mayor\u00eda menores de 2 bar. La ley de escala correspondiente indica un aumento de \u00e9stos con el momento s\u00edsmico. Los radios de fuente obtenidos son todos superiores a 180 metros, a pesar de haber considerado eventos de magnitud menor de 2.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Parametros de fuente de los terremotos del mar de alboran.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Parametros de fuente de los terremotos del mar de alboran. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Taoufik Mourabit <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 13\/05\/1998<\/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>Jos\u00e9 Morales soto (vocal)<\/li>\n<li>Antonio Posadas chinchilla (vocal)<\/li>\n<li>m.dolores Romacho romero (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Taoufik Mourabit Se han analizado terremotos y microterremotos ocurridos en el mar de albor\u00e1n y zonas lim\u00edtrofes [&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":[27,1033,4067],"tags":[22124,15678,4070,22122,4072,99325],"class_list":["post-38139","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geofisica","category-sismologia-y-prospeccion-sismica","tag-antonio-posadas-chinchilla","tag-francisco-de-asis-vidal-sanchez","tag-jose-antonio-canas-torres","tag-jose-morales-soto","tag-m-dolores-romacho-romero","tag-taoufik-mourabit"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/38139","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=38139"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/38139\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=38139"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=38139"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=38139"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}