{"id":10091,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1996\/01\/01\/la-actividad-neotectonica-en-las-cadenas-costeras-catalanas\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"la-actividad-neotectonica-en-las-cadenas-costeras-catalanas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-actividad-neotectonica-en-las-cadenas-costeras-catalanas\/","title":{"rendered":"La actividad neotectonica en las cadenas costeras catalanas."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Eulalia Masana Closa <\/strong><\/h2>\n<p>La sismicidad instrumental e historica indica que en un periodo de 1.000 a\u00f1os la zona de las cadenas costeras catalanas ha experimentado solamente algun sismo que causo da\u00f1os (intensidad vii). Esto me ha motivado a un estudio neotectonico de un periodo mas amplio -desde el mioceno superior- para caracterizar la tectonica mas reciente de la zona. He utilizado cuatro fuentes de datos: bibliografia, fotointerpretacion, campo y gabinete, a partir de las cuales he realizado un analisis geomorfologico, estructural, de la paleosismicidad. Los resultados indican que la zona ha experimentado actividad neotectonica suave extensiva -de tipo vertical-, en continuidad con la extension iniciada en el mioceno inferior, y que esta actividad se ha concentrado en la mitad meridional del area, coincidiendo con la zona con menor sismicidad. En segundo lugar concluyo que aunque la sismicidad historica e instrumental no indica terremotos catastroficos, el analisis de la paleosismicidad muestra una tectonica activa en la zona. Asi describo cuatro escarpes de falla entre los que destaca el de mont-roig, producido por una falla activa para la cual se estima un periodo de retorno de pocos miles de a\u00f1os.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La actividad neotectonica en las cadenas costeras catalanas.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La actividad neotectonica en las cadenas costeras catalanas. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Eulalia Masana Closa <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Joan Guimera Rosso<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Pere Santanach Prat <\/li>\n<li>Ram\u00f3n Juli\u00e1 Brugu\u00e9s (vocal)<\/li>\n<li>Daniela Pantosti (vocal)<\/li>\n<li>Antonio Estevez  Rubio (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Eulalia Masana Closa La sismicidad instrumental e historica indica que en un periodo de 1.000 a\u00f1os la [&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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