{"id":5120,"date":"1995-01-01T00:00:00","date_gmt":"1995-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1995\/01\/01\/sismicidad-y-tectonica-en-el-limite-de-placas-del-caribe-noreste-de-venezuela-e-hispaniola\/"},"modified":"1995-01-01T00:00:00","modified_gmt":"1995-01-01T00:00:00","slug":"sismicidad-y-tectonica-en-el-limite-de-placas-del-caribe-noreste-de-venezuela-e-hispaniola","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/sismicidad-y-tectonica-en-el-limite-de-placas-del-caribe-noreste-de-venezuela-e-hispaniola\/","title":{"rendered":"Sismicidad y tectonica en el limite de placas del caribe: noreste de venezuela e hispaniola."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Antonio Villase\u00f1or Hidalgo <\/strong><\/h2>\n<p>Se ha realizado el analisis sismotectonico de dos zonas del limite de placas del caribe. Para el ne de venezuela se han obtenido hipocentros y mecanismos focales de terremotos locales detectados por una red temporal de microsismicidad. Tambien se han determinado los parametros focales para los terremotos de mayor magnitud ocurridos en el ne de venezuela con posterioridad a 1963 mediante el metodo de inversion de forma de ondas internas. Del analisis de estos datos se deduce que el principal limite tectonico en la zona es la falla del pilar, la cual se comporta como una falla de desgarre dextra.  se ha estudiado tambien el gran terremoto del 4 de agosto de 1946 y su serie de replicas, ocurrido en el ne de hispaniola y que constituye el mayor terremoto registrado instrumentalmente en el limite de placas del caribe. Se han relocalizado todos los terremotos de la serie y se han calculado mecanismos focales para los eventos de mayor magnitud.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Sismicidad y tectonica en el limite de placas del caribe: noreste de venezuela e hispaniola.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Sismicidad y tectonica en el limite de placas del caribe: noreste de venezuela e hispaniola. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Antonio Villase\u00f1or Hidalgo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1995<\/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>Enric Banda Tarradellas<\/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>Josep Gallart Muset (vocal)<\/li>\n<li>Julio Mezcua Rodr\u00edguez (vocal)<\/li>\n<li>Francisco De Asis Vidal Sanchez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Antonio Villase\u00f1or Hidalgo Se ha realizado el analisis sismotectonico de dos zonas del limite de placas del [&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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