{"id":75353,"date":"2005-04-07T00:00:00","date_gmt":"2005-04-07T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/cenozoic-seismic-stratigraphy-of-the-sw-galician-shelf-comparison-with-canterbury-shelf-se-new-zealand-during-the-quaternary\/"},"modified":"2005-04-07T00:00:00","modified_gmt":"2005-04-07T00:00:00","slug":"cenozoic-seismic-stratigraphy-of-the-sw-galician-shelf-comparison-with-canterbury-shelf-se-new-zealand-during-the-quaternary","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/cenozoic-seismic-stratigraphy-of-the-sw-galician-shelf-comparison-with-canterbury-shelf-se-new-zealand-during-the-quaternary\/","title":{"rendered":"Cenozoic seismic stratigraphy of the sw galician shelf. comparison with canterbury shelf (se new zealand) during the quaternary"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Fern\u00e1ndez Ferr\u00edn Carlos Alberto <\/strong><\/h2>\n<p>1. Estratigraf\u00eda s\u00edsmica de la plataforma continental gallega durante el cenozoico.  se han identificado nueve secuencias deposicionales de alta resoluci\u00f3n relacionadas con ciclos de segundo (s1,s2, s3, y s4) y tercer (sq4.1, sq 4.2, sq 4.3, sq 4.4, y sq 4.5) en el relleno sedimentario de la plataforma suroeste de galicia. Las secuencias principales est\u00e1n separadas por superficies de discontinuidad relacionadas con los cambios eust\u00e1ticos y tect\u00f3nicos m\u00e1s importantes acaecidos en la zona desde la apertura del atl\u00e1ntico. Las secuencias que corresponden a los ciclos 3etorder est\u00e1n separadas por cinco discontinuidades que corresponden a los cambios relativos m\u00e1s dr\u00e1sticos del nivel del mar que afectaron al atl\u00e1ntico desde el mioceno superiorhasta la actualidad.  2. Estratigraf\u00eda s\u00edsmica de la plataforma gallega durante el cuaternario  el an\u00e1lisis s\u00edsmico de registros de muy alta resoluci\u00f3n nos ha permitido reconocer y cartografiar la superficie erosiva relacionada con la regresi\u00f3n del w\u00ed\u00bcrm y \u00faltimo m\u00e1ximo glaciar (lgm), en las r\u00edas baixas y plataforma continental adyacente. Esta superficie representa una importante discontinuidad desarrollada directamente sobre materiales pleistocenos dentro de las r\u00edas y en un porcentaje elevado de la plataforma. Sin embargo, hay lugares donde esta discontinuidad se desarrolla directamente sobre materiales terciarios e incluso mesozoicos. La profundidad por debajo del fondo a la que se encuentra esta superficie se ha medido, y esto nos ha permitido  elaborar una paleobatimetr\u00eda para el lgm y un mapa de isopacas de la unidad s\u00edsmica desarrollada por encima.  el mapa morfosedimentario de la plataforma gallega se ha confeccionado a partir de la cartograf\u00eda de datos granulom\u00e9tricos, teniendo en cuenta la batimetr\u00eda de detalle de la zona, el mapa de pendientes de alta resoluci\u00f3n, y los patrones sonogr\u00e1ficos (sonar de barrido lateral) disponibles para el \u00e1rea de estudio.  3. G<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Cenozoic seismic stratigraphy of the sw galician shelf. comparison with canterbury shelf (se new zealand) during the quaternary<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Cenozoic seismic stratigraphy of the sw galician shelf. comparison with canterbury shelf (se new zealand) during the quaternary <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Fern\u00e1ndez Ferr\u00edn Carlos Alberto <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Vigo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 04\/07\/2005<\/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>Soledad Garc\u00eda Gil<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: lorenzo Vilas minondo <\/li>\n<li>gemma Ercilla zarraga (vocal)<\/li>\n<li>bilal Haq (vocal)<\/li>\n<li>Mar\u00eda no Marzo carpio (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Fern\u00e1ndez Ferr\u00edn Carlos Alberto 1. Estratigraf\u00eda s\u00edsmica de la plataforma continental gallega durante el cenozoico. se han [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[27,245,953,18657],"tags":[162938,162937,138028,5043,16636,51195],"class_list":["post-75353","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-estratigrafia","category-geologia","category-vigo","tag-bilal-haq","tag-fernandez-ferrin-carlos-alberto","tag-gemma-ercilla-zarraga","tag-lorenzo-vilas-minondo","tag-maria-no-marzo-carpio","tag-soledad-garcia-gil"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/75353","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=75353"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/75353\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=75353"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=75353"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=75353"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}