{"id":46569,"date":"2019-11-27T16:14:25","date_gmt":"2019-11-27T16:14:25","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/los-yacimientos-de-hierro-de-la-comarca-del-marquesado-del-zenete-alquife-y-las-piletas-granada-cordilleras-beticas\/"},"modified":"2019-11-27T16:14:25","modified_gmt":"2019-11-27T16:14:25","slug":"los-yacimientos-de-hierro-de-la-comarca-del-marquesado-del-zenete-alquife-y-las-piletas-granada-cordilleras-beticas","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/los-yacimientos-de-hierro-de-la-comarca-del-marquesado-del-zenete-alquife-y-las-piletas-granada-cordilleras-beticas\/","title":{"rendered":"Los yacimientos de hierro de la comarca del marquesado del zenete: alquife y las piletas (granada, cordilleras beticas)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jose Torres Ruiz <\/strong><\/h2>\n<p>Los yacimientos de hierro de la comarca del marquesado enclavados en materiales del complejo nevado-filabride (zona betica s.Str.) Estan constituidos por una asociacion espacial de diversas mineralizaciones con caracteristicas diferentes y son el resultado final de la evolucion sufrida por unas primitivas mineralizaciones de caracter sedimentario y\/o diagenetico precoz de edad triasica. Las menas principales estan constituidas por oxidos  oxihidroxidos  carbonatos y sulfuros de fe y por peque\u00f1as cantidades de oxidos y carbonatos de mn. Se distinguen dos grupos de mineralizaciones  unas intercaladas en rocas peliticas y otras en relacion con rocas carbontatadas siendo estas ultimas las mas importantes  las mineralizaciones primarias se formaron en una cuenca restringida tipo  lagoon  con una diferenciacion lateral y vertical en facies mineralogicas: facies de oxidos facies de carbonatos y facies mixta de magnetita y pirita. Con posterioridad sufren una evolucion paralela al contexto geologico. Son afectadas por el metamorfismo alpino y por importantes procesos de meteorizacion en la zona de oxidacion siendo estos ultimos procesos muy intensos en las mineralizaciones de facies de carbonatos en donde las transformaciones estan condicionadas por un regimen hidrogeologico carstico. Parte de la zona de oxidacion es erosionada dando lugar a depositos de tipo carstico. La principal fuente del hierro deriva de meteorizacion continental<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Los yacimientos de hierro de la comarca del marquesado del zenete: alquife y las piletas (granada, cordilleras beticas).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Los yacimientos de hierro de la comarca del marquesado del zenete: alquife y las piletas (granada, cordilleras beticas). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jose Torres Ruiz <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Granada<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1980<\/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>ali Fenoll Hach<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Purificacion Fenoll Hach-ali <\/li>\n<li>Antonio Arribas Moreno (vocal)<\/li>\n<li> Fontbote Mussolas Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<li>Manuel Rodr\u00edguez Gallego (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jose Torres Ruiz Los yacimientos de hierro de la comarca del marquesado enclavados en materiales del complejo [&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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