{"id":2224,"date":"1994-01-01T00:00:00","date_gmt":"1994-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/1994\/01\/01\/geologia-y-metalogenia-de-las-mineralizaciones-sedimentarias-de-hierro-ordovicicas-del-sinforme-de-alcanices-flanco-s-zamora\/"},"modified":"1994-01-01T00:00:00","modified_gmt":"1994-01-01T00:00:00","slug":"geologia-y-metalogenia-de-las-mineralizaciones-sedimentarias-de-hierro-ordovicicas-del-sinforme-de-alcanices-flanco-s-zamora","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/geologia-y-metalogenia-de-las-mineralizaciones-sedimentarias-de-hierro-ordovicicas-del-sinforme-de-alcanices-flanco-s-zamora\/","title":{"rendered":"Geolog\u00eda y metalogenia de las mineralizaciones sedimentarias de hierro ordovicicas del sinforme de alca\u00f1ices (flanco s, zamora)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Agustina Fernandez Fernandez <\/strong><\/h2>\n<p>En este trabajo se ha realizado un estudio de las caracteristicas morfologicas, texto estructurales, mineralogicas y quimicas de las mineralizaciones de fe que afloran en el flanco s del sinforme de alca\u00f1ices, asi como de los materiales ordovicicos a los cuales estan asociadas. Se ha hecho un analisis de la fuente del fe:  areas continentales emergidas durante el arenig-llanvirn, del medio de transporte: fundamentalmente como oxido ferrico adsorvido en la superficie de las particulas arcillosas y de la cuenca de deposito: medio marino somero de plataforma continental, la cual, a escala global, formaba parte de la amplia plataforma situada en el margen n del continente de gondwana durante el ordovico, en latitudes proximas al polo s y en un ambiente geotectonico de margen pasivo.  las mineralizaciones de fe, estratigraficamente, se encuentran interestratificadas en el miembro superior de la fm. Cuarcitas del pielgo (arenig) y presentan una estructura bandeada con alternancia de lechos esencialmente ferriferos cuarciticos, chamositicos y chamositicos-biotiticos y, mineralogicamente, estan constituidos por magnetita, hematites, chamosita, biotita y apatito como minerales esenciales e ilmenita, rutilo, grafito, pirita, circon y turmalina como accesorios.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Geolog\u00eda y metalogenia de las mineralizaciones sedimentarias de hierro ordovicicas del sinforme de alca\u00f1ices (flanco s, zamora).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Geolog\u00eda y metalogenia de las mineralizaciones sedimentarias de hierro ordovicicas del sinforme de alca\u00f1ices (flanco s, zamora). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Agustina Fernandez Fernandez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/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> Moro Benito M. Candelas<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Rosario Lunar <\/li>\n<li>Enrique Mart\u00ednez Garc\u00eda (vocal)<\/li>\n<li>Jacques Chauvel Jean (vocal)<\/li>\n<li>Jos\u00e9 Torres Ruiz (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Agustina Fernandez Fernandez En este trabajo se ha realizado un estudio de las caracteristicas morfologicas, texto estructurales, [&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":[27,953,9386,3857,3612],"tags":[9529,9532,9533,9534,9530,9531],"class_list":["post-2224","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-salamanca","category-sedimentologia","category-yacimientos-minerales","tag-agustina-fernandez-fernandez","tag-enrique-Martinez-garcia","tag-jacques-chauvel-jean","tag-jose-torres-ruiz","tag-moro-benito-m-candelas","tag-rosario-lunar"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/2224","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=2224"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/2224\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=2224"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=2224"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=2224"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}