{"id":53335,"date":"2018-03-09T22:41:00","date_gmt":"2018-03-09T22:41:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-estructura-del-sector-meridional-de-la-republica-dominicana-una-aproximacion-a-su-evolucion-geodinamica-durante-el-cenozoico\/"},"modified":"2018-03-09T22:41:00","modified_gmt":"2018-03-09T22:41:00","slug":"la-estructura-del-sector-meridional-de-la-republica-dominicana-una-aproximacion-a-su-evolucion-geodinamica-durante-el-cenozoico","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-estructura-del-sector-meridional-de-la-republica-dominicana-una-aproximacion-a-su-evolucion-geodinamica-durante-el-cenozoico\/","title":{"rendered":"La estructura del sector meridional de la rep\u00fablica dominicana. una aproximaci\u00f3n a su evoluci\u00f3n geodin\u00e1mica durante el cenozoico"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Hernaiz Huerta Pedro Pablo <\/strong><\/h2>\n<p>La tesis describe la estratigraf\u00eda y la estructura cenozoica de los siguientes dominios del sector meridional de la rep\u00fablica dominicana, de ne a so:     1,- un basamento de arco de isla, formado, en su parte oriental, por las unidades antiguas (\u00c2\u00bfarco de isla primitivo del cret\u00e1cico inferior?) Y metam\u00f3rficas del cintur\u00f3n intermedio, las cuales se disponen en bandas de direcci\u00f3n no-se subparalelas a la zona de falla de la espa\u00f1ola; y en su parte occidental, por la fm. Tireo, que se identifica como el principal producto del magnetismo del arco durante el cret\u00e1cico superior y tiene una estructura interna en escamas con vergencia al s o se.     2,- la cuenca trasera del arco de isla, de edad fundamentalmente pale\u00f3gena y naturaleza esencialmente turbid\u00edtica, que fue posteriormente deformada en un cintur\u00f3n de pliegues y cabalgamientos (cintur\u00f3n de peralta) de similar vergencia y desplazamiento al s o se.     3,- las sierras de neiba, mart\u00edn garc\u00eda y bahoruco (margen norte), que constituyen grandes estructuras anticlinales o anticlinoriales de direcci\u00f3n ne-so a ono-ese limitadas por fallas inversas o cabalgamientos de alto \u00e1ngulo y est\u00e1n formadas pro potentes series carbonatadas pale\u00f3genas de plataforma (con un intervalo volc\u00e1nico de relevancia en la sierra de neiba) que se depositaron sobre un sustrato del cret\u00e1cico superior con afinidades litol\u00f3gicas y geoqu\u00edmicas del plateau oce\u00e1nico del caribe.     4,- las cuencas ne\u00f3genas internas de san juan-azua y enriquillo que se generaron como consecuencia del levantamiento de los relieves circundantes y su relleno consiste en potentes series fundamentalmente detr\u00edticas, (con un importante episodio evapor\u00edtico  en la cuenca de enriquillo) de car\u00e1cter sintect\u00f3nico y tendencia somerizante (ambientes marinos en la bases y continentales a techo).     la tesis propone un modelo estructural para el conjunto de la zona de estuido que se resume en los siguientes puntos:     1,- la deformaci\u00f3n es<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La estructura del sector meridional de la rep\u00fablica dominicana. una aproximaci\u00f3n a su evoluci\u00f3n geodin\u00e1mica durante el cenozoico<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La estructura del sector meridional de la rep\u00fablica dominicana. una aproximaci\u00f3n a su evoluci\u00f3n geodin\u00e1mica durante el cenozoico <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Hernaiz Huerta Pedro Pablo <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 22\/06\/2006<\/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> Escuder Viruete JavierDel Pilar<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: ram\u00f3n Vegas mart\u00ednez <\/li>\n<li>Luis roberto Rodr\u00edguez fern\u00e1ndez (vocal)<\/li>\n<li>Andr\u00e9s Perez estaun (vocal)<\/li>\n<li>gabriel Guti\u00e9rrez alonso (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Hernaiz Huerta Pedro Pablo La tesis describe la estratigraf\u00eda y la estructura cenozoica de los siguientes dominios [&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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