{"id":39582,"date":"1999-01-01T00:00:00","date_gmt":"1999-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/metodo-para-la-inversion-del-tensor-momento-sismico-terremotos-del-sur-de-espana\/"},"modified":"1999-01-01T00:00:00","modified_gmt":"1999-01-01T00:00:00","slug":"metodo-para-la-inversion-del-tensor-momento-sismico-terremotos-del-sur-de-espana","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/metodo-para-la-inversion-del-tensor-momento-sismico-terremotos-del-sur-de-espana\/","title":{"rendered":"Metodo para la inversion del tensor momento sismico. terremotos del sur de espa\u00f1a."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Mar\u00eda  Pilar Coca Llanos <\/strong><\/h2>\n<p>Se ha desarrollado un m\u00e9todo de inversi\u00f3n lineal que permite obtener las componentes del tensor momento s\u00edsmico para terremotos registrados a distancias regionales. La ventaja de utilizar el tensor momento s\u00edsmico para calcular el mecanismo focal de los terremotos, consiste en que \u00e9ste representa una forma de ruptura general. A partir del tensor momento s\u00edsmico se puede calcular el patr\u00f3n de radiaci\u00f3n (doble par y clvd) y la funci\u00f3n temporal de la fuente s\u00edsmica. Adem\u00e1s, se realiza un estudio de los errores cometidos en las magnitudes calculadas.  con el fin comprobar el buen funcionamiento del m\u00e9todo, se ha realizado un estudio detallado de casos te\u00f3ricos: mecanismo focal de desgarre, vertical y deslizamiento en direcci\u00f3n del buzamiento, con porcentajes de clvd entre 0 y 35%, realizando inversiones a diferentes profundidades.  tras comprobar el correcto funcionamiento del m\u00e9todo, \u00e9ste se ha aplicado a cuatro terremotos de profundidad intermedia espa\u00f1a, y un terremoto profundo (h=637km). se han utilizado sismogramas digitales de velocidad de la onda p directa, registrados a distancias regionales en las estaciones de la red s\u00edsmica nacional. para los terremotos a profundidad intermedia, la soluci\u00f3n obtenida para tres de ellos tiene una componente de clvd peque\u00f1a, menor al 6%, lo cual supone que su mecanismo focal corresponde a un doble par, para el cuarto terremoto intermedio se obtuvo que su porcentaje de clvd era del 20%. La soluci\u00f3n obtenida para el terremoto profundo muestra un 10% de clvd, que siendo peque\u00f1o, es fundamental para ajustar las polaridades de las estaciones utilizadas en la inversi\u00f3n. As\u00ed mismo se ha realizado un estudio detallado de la profundidad de los terremotos.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Metodo para la inversion del tensor momento sismico. terremotos del sur de espa\u00f1a.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Metodo para la inversion del tensor momento sismico. terremotos del sur de espa\u00f1a. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Mar\u00eda  Pilar Coca Llanos <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1999<\/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>Elisa Buforn Peir\u00f3<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal:  Fernandez-ra\u00f1ada y menendez de luarca Antonio <\/li>\n<li>Antonio  Mar\u00eda Correig blanchar (vocal)<\/li>\n<li>agust\u00edn Ud\u00edas vallina (vocal)<\/li>\n<li>raul Madariaga (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Mar\u00eda Pilar Coca Llanos Se ha desarrollado un m\u00e9todo de inversi\u00f3n lineal que permite obtener las componentes [&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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