{"id":1472,"date":"1994-01-01T00:00:00","date_gmt":"1994-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1994\/01\/01\/estudio-paleomagnetico-y-magnetoestratigrafico-del-periodo-jurasico-en-el-sistema-iberico\/"},"modified":"1994-01-01T00:00:00","modified_gmt":"1994-01-01T00:00:00","slug":"estudio-paleomagnetico-y-magnetoestratigrafico-del-periodo-jurasico-en-el-sistema-iberico","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-paleomagnetico-y-magnetoestratigrafico-del-periodo-jurasico-en-el-sistema-iberico\/","title":{"rendered":"Estudio paleomagnetico y magnetoestratigrafico del periodo jurasico en el sistema iberico"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Teresa Juarez Colera <\/strong><\/h2>\n<p>Esta tesis ha consistido en un estudio mineralogico, paleomagnetico y magnetoestratigrafico en calizas de edad oxfordiense (jurasico superior), recogidas en diversos emplazamientos dentro del sistema iberico. La mineralogia magnetica encontrada esta compuesta principalmente por magnetita con diferentes rangos de campo coercitivo y ocasionalmente por goetita. Los resultados paleomagneticos reflejan la presencia de dos componentes en la imanacion, ambas diferenciables del campo magnetico actual. Estas corresponden a la componente primaria de la imanacion y a una reimanacion de edad cretacica. Las muestras que contienen goetita presentan una tercera componente paleomagnetica correspondiente, probablemente, tambien a una reimancion de edad cretacica.  la rotacion entre la componente primaria y la reimanacion cretacica refleja el giro de la placa iberica entre ambas epocas de adquisicion.  por otra parte las diferencias direccionales encontradas entre unas regiones y otras del sistema iberico indican que han tenido lugar rotaciones diferenciales de bloques dentro de la cordillera.  las direcciones obtenidas para la componente primaria reflejan los cambios de polaridad del campo magnetico terrestre durante el oxfordiense medio-superior. Los resultados obtenidos pueden considerarse como el patron de polaridades del campo magnetico terrestre para dicha epoca.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio paleomagnetico y magnetoestratigrafico del periodo jurasico en el sistema iberico<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio paleomagnetico y magnetoestratigrafico del periodo jurasico en el sistema iberico <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Teresa Juarez Colera <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1994<\/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> Osete Lopez M. Luisa<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Agust\u00edn Ud\u00edas Vallina <\/li>\n<li>Guillermo Melendez (vocal)<\/li>\n<li> Zijderveld (vocal)<\/li>\n<li>Mar\u00eda Pares Jose (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Teresa Juarez Colera Esta tesis ha consistido en un estudio mineralogico, paleomagnetico y magnetoestratigrafico en calizas de [&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":[27,1033,6376],"tags":[5017,6379,6381,6378,6377,6380],"class_list":["post-1472","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geofisica","category-paleomagnetismo","tag-agustin-udias-vallina","tag-guillermo-melendez","tag-maria-pares-jose","tag-osete-lopez-m-luisa","tag-teresa-juarez-colera","tag-zijderveld"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/1472","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=1472"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/1472\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=1472"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=1472"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=1472"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}