{"id":43745,"date":"2018-07-06T19:39:51","date_gmt":"2018-07-06T19:39:51","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/genesis-constitucion-y-propiedades-de-yacimientos-de-caolin-de-sierra-morena-occidental\/"},"modified":"2018-07-06T19:39:51","modified_gmt":"2018-07-06T19:39:51","slug":"genesis-constitucion-y-propiedades-de-yacimientos-de-caolin-de-sierra-morena-occidental","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/quimica\/genesis-constitucion-y-propiedades-de-yacimientos-de-caolin-de-sierra-morena-occidental\/","title":{"rendered":"Genesis, constitucion y propiedades de yacimientos de caolin de sierra morena occidental."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Juan Poyato Ferrera <\/strong><\/h2>\n<p>Se ha estudiado la mineralogia y genesis de seis yacimientos de caolin situados en las provincias de huelva y sevilla. En dos de estos yacimientos  el de riotinto y traslasierra (huelva) el caolin se ha originado a partir de rocas volcanicas  en el primer caso por un lixiviado sulfurico y en el segundo por actividad hidrotermal. En los yacimientos de s. Telmo y sta barbara (huelva) y en el de el alamo (sevilla)  la alteracion a caolin se ha efectuado sobre pizarras paleozoicas asignandose al primero un origen meteorico y al segundo un origen hidrotermal. En el yacimiento de almonaster  el material caolinitico se ha originado por alteracion meteorica de una diorita  estando constituido por una caolinita de baja cristalinidad. Se dan tambien en este estudio datos tecnologicos para el mejor aprovechamiento ceramico de los materiales de estos yacimientos<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Genesis, constitucion y propiedades de yacimientos de caolin de sierra morena occidental.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Genesis, constitucion y propiedades de yacimientos de caolin de sierra morena occidental. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Juan Poyato Ferrera <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Sevilla<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1977<\/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>Francisco Gonzalez Garcia<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Francisco Gonzalez Garcia <\/li>\n<li>Guillermo Munuera Contreras (vocal)<\/li>\n<li>Enrique Gutierrez Rios (vocal)<\/li>\n<li>Jos\u00e9 Mar\u00eda Trillo De Leyva (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Juan Poyato Ferrera Se ha estudiado la mineralogia y genesis de seis yacimientos de caolin situados en [&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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