{"id":80672,"date":"2018-03-10T00:04:27","date_gmt":"2018-03-10T00:04:27","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructura-de-la-corteza-y-del-manto-litosferico-en-la-zona-de-colision-entre-la-placa-africana-y-la-peninsula-iberica\/"},"modified":"2018-03-10T00:04:27","modified_gmt":"2018-03-10T00:04:27","slug":"estructura-de-la-corteza-y-del-manto-litosferico-en-la-zona-de-colision-entre-la-placa-africana-y-la-peninsula-iberica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estructura-de-la-corteza-y-del-manto-litosferico-en-la-zona-de-colision-entre-la-placa-africana-y-la-peninsula-iberica\/","title":{"rendered":"Estructura de la corteza y del manto litosf\u00e9rico en la zona de colisi\u00f3n entre la placa africana y la peninsula ib\u00e9rica"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Gurr\u00eda Celimendiz Ezequiel Mar\u00eda no <\/strong><\/h2>\n<p>La zona de colisi\u00f3n entre la placa tect\u00f3nica africana y la pen\u00ednsula ib\u00e9rica, es de especial inter\u00e9s por contener la mayor parte de la sismicidad que afecta a la pen\u00ednsula ib\u00e9rica y tambi\u00e9n por ser una zona cuya evoluci\u00f3n geol\u00f3gica ha sido compleja. Esta zona contiene el mar de albor\u00e1n que actualmente centra la atenci\u00f3n de la comunidad geol\u00f3gica y geof\u00edsica internacional, por considerar que su evoluci\u00f3n es paradigm\u00e1tica del proceso de delaminaci\u00f3n litosf\u00e9rica, por el cual se desprende y hunde en el manto parte de lalitosfera. con la intenci\u00f3n de contribuir al conocimiento de la estructura de velocidad s\u00edsmica de la corteza y del manto litosf\u00e9rico en la zona, se ha llevado a cabo un ambicioso estudio geof\u00edsico de la regi\u00f3n partiendo de dos conjunto de datos s\u00edsmicos distintos. El primer estudio se ha realizado utilizando ondas s\u00edsmicas superficiales del t\u00edpo rayleigh con lo que se logra obtener informaci\u00f3n  de la estructura litosf\u00e9rica de parte de la cuenca de albor\u00e1n, y parte de la cuenca de argelia (o sur balear). La escasa cobertura de la zona de estudio por las trayectorias epicentro -estaci\u00f3n del conjunto de datos utilizado, sol\u00e1mente permite obtener resultados de baja resoluci\u00f3n espacial, pero s\u00ed sirve para indicar la profundidad media del moho y tambi\u00e9n revela las velocidades s\u00edsmicas caracter\u00edsticas de la corteza inferior y el manto litosf\u00e9rico. Tambi\u00e9n se ha procedido a regionalizar las velocidades de grupo observadas por inversi\u00f3n lineal de los tiempos de propagaci\u00f3n de las ondas, con la idea de obtener valores locales y comparar estos resultados con los conseguidos anteriormente. En el segundo estudio utilizamos los tiempos de recorrido de las primeras llegadas de las ondas p y s del cat\u00e1logo s\u00edsmico del instituto geogr\u00e1fico nacional, para realizar una tomograf\u00eda de corteza y del manto litosf\u00e9rico. La distribuci\u00f3n de sismicidad y estaciones s\u00edsmicas del conjunto de datos nos permite ob<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estructura de la corteza y del manto litosf\u00e9rico en la zona de colisi\u00f3n entre la placa africana y la peninsula ib\u00e9rica<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estructura de la corteza y del manto litosf\u00e9rico en la zona de colisi\u00f3n entre la placa africana y la peninsula ib\u00e9rica <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Gurr\u00eda Celimendiz Ezequiel Mar\u00eda no <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 21\/09\/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>Jos\u00e9 Ignacio Badal Nicolas<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Antonio  Mar\u00eda Correig blanchar <\/li>\n<li> Blanco s\u00e1nchez Mar\u00eda  Jos\u00e9 (vocal)<\/li>\n<li> Da\u00f1obeitia canales Juan  Jos\u00e9 (vocal)<\/li>\n<li>diego Cordoba barba (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gurr\u00eda Celimendiz Ezequiel Mar\u00eda no La zona de colisi\u00f3n entre la placa tect\u00f3nica africana y la pen\u00ednsula [&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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