{"id":129539,"date":"1996-01-01T00:00:00","date_gmt":"1996-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estructura-y-mineralizaciones-auriferas-del-area-de-tomino-pontevedra\/"},"modified":"1996-01-01T00:00:00","modified_gmt":"1996-01-01T00:00:00","slug":"estructura-y-mineralizaciones-auriferas-del-area-de-tomino-pontevedra","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estructura-y-mineralizaciones-auriferas-del-area-de-tomino-pontevedra\/","title":{"rendered":"Estructura y mineralizaciones auriferas del area de tomi\u00f1o (pontevedra)."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Toyos Saenz De Miera Jos\u00e9 M. <\/strong><\/h2>\n<p>En el area de tomi\u00f1o aflora una estrecha banda de rocas metasedimentarias orientada en direccion n-s, bordeada por rocas graniticas. El estudio realizado se ha centrado en la litoestratigrafia de dicha banda, en su estructura, y en las mineralizaciones auriferas, las cuales se encuentran en estrecha relacion con determinadas estructuras. Se han diferenciado seis unidades litoestratigraficas que componen una sucesion siliciclastica con un espesor total aparente de 2.000 m, con edades probablemente comprendidas entre el cambrico y el silurico. La deformacion producida durante la orogenia varisca ha dado lugar a pliegues a distintas escalas que corresponden a dos generaciones principales, y diversas bandas de cizalla longitudinales subverticales, junto con una serie de fallas mas tardias. Las mineralizaciones consisten basicamente en filones de cuarzo con sulfuros a los que se encuentra asociado el au. Se localizan principalmente en dos tipos de estructuras tardias: venas de cuarzo intragraniticas y zonas de cizalla en la banda metasedimentaria. Las caracteristicas que presentan son propias de mineralizaciones auriferas filonianas mesotermales.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estructura y mineralizaciones auriferas del area de tomi\u00f1o (pontevedra).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estructura y mineralizaciones auriferas del area de tomi\u00f1o (pontevedra). <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Toyos Saenz De Miera Jos\u00e9 M. <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Oviedo<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1996<\/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>Andres Perez Estaun<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Alberto Marcos Vallaure <\/li>\n<li> Martinez Catalan Jos\u00e9 Ramon (vocal)<\/li>\n<li>Antonio Ribeiro (vocal)<\/li>\n<li>Fern\u00e1ndo Tornos Arroyo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Toyos Saenz De Miera Jos\u00e9 M. En el area de tomi\u00f1o aflora una estrecha banda de rocas [&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":[27,953,3435,232,8846],"tags":[9049,9050,9052,13176,9051,242920],"class_list":["post-129539","post","type-post","status-publish","format-standard","hentry","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-estructural","category-mineralogia","category-oviedo","tag-alberto-marcos-vallaure","tag-andres-perez-estaun","tag-antonio-ribeiro","tag-fernando-tornos-arroyo","tag-Martinez-catalan-jose-ramon","tag-toyos-saenz-de-miera-jose-m"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/129539","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=129539"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/129539\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=129539"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=129539"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=129539"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}