{"id":100868,"date":"2018-03-11T10:22:30","date_gmt":"2018-03-11T10:22:30","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/sedimentologa%c2%ada-silicificaciones-y-otros-procesos-diageneticos-en-las-unidades-intermedia-y-superior-del-mioceno-de-la-cuenca-de-madrid-zo-nas-ne-nw-y-w\/"},"modified":"2018-03-11T10:22:30","modified_gmt":"2018-03-11T10:22:30","slug":"sedimentologa%c2%ada-silicificaciones-y-otros-procesos-diageneticos-en-las-unidades-intermedia-y-superior-del-mioceno-de-la-cuenca-de-madrid-zo-nas-ne-nw-y-w","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/sedimentologa%c2%ada-silicificaciones-y-otros-procesos-diageneticos-en-las-unidades-intermedia-y-superior-del-mioceno-de-la-cuenca-de-madrid-zo-nas-ne-nw-y-w\/","title":{"rendered":"Sedimentolog\u00eda, silicificaciones y otros procesos diagen\u00e9ticos en las unidades intermedia y superior del mioceno de la cuenca de Madrid (zo-nas ne, nw y w)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jos\u00e9 Luis Perez Jimenez <\/strong><\/h2>\n<p>Las rocas del mioceno de la cuenca de Madrid se formaron en diferentes ambientes sedimentarios. En estos ambientes se produjeron silicificaciones y otros procesos diagen\u00e9ticos tempranos. los ambientes sedimentarios vinculados a procesos de silicifica ci\u00f3n en la zona ne de la cuenca son: ambiente palustre carbon\u00e1tico con sepiolita y palustre evapor\u00edtico. En la zona nw son: lacustre somero y de margen lacustre. En la zona w son: palustre sepiol\u00edtico\/llanura lut\u00edtica con calcretas; palustre-lacustre  con rasgos k\u00e1rsticos; fluvial; charcas diatom\u00edticas y rellenos de cavidades de colapso. Las secuencias sedimentarias de los distintos ambientes ha sido establecida y en cada una de las tres zonas se ha propuesto un modelo sedimentario. los procesos de silicificaci\u00f3n afectan a carbonatos, lutitas, yesos y diatomitas. Junto a ellos, otros procesos diagen\u00e9ticos reconocidos son: autig\u00e9nesis de sulfatos, arcillas, tectosilicatos y zeolitas; cementaci\u00f3n de calcita y estroncianita; calcitizaci\u00f3n; dolo mitizaci\u00f3n y karstificaci\u00f3n-formaci\u00f3n de espeleotemas. La secuencia de procesos diagen\u00e9ticos ha sido establecida en relaci\u00f3n con los ambientes sedimentarios reconocidos. los principales procesos diagen\u00e9ticos del ambiente palustre\/lacustre somero carb on\u00e1tico de la zona ne son dedolomitizaci\u00f3n y formaci\u00f3n de silcretas, en un contexto evapor\u00edtico y con fluctuaciones del nivel fre\u00e1tico. Por el contrario, en las zonas nw y w predomina la formaci\u00f3n de silcretas en llanuras lut\u00edticas con autig\u00e9nesis de  esmectitas. En las llanuras lut\u00edticas de la zona w tambi\u00e9n fue extensiva la formaci\u00f3n de calcretas\/dolocretas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Sedimentolog\u00eda, silicificaciones y otros procesos diagen\u00e9ticos en las unidades intermedia y superior del mioceno de la cuenca de Madrid (zo-nas ne, nw y w)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Sedimentolog\u00eda, silicificaciones y otros procesos diagen\u00e9ticos en las unidades intermedia y superior del mioceno de la cuenca de Madrid (zo-nas ne, nw y w) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jos\u00e9 Luis Perez Jimenez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 14\/05\/2010<\/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>Ana Mar\u00eda Alonso Zarza<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: rafaela Marfil perez <\/li>\n<li>Jos\u00e9 Javier Elorza zandueta (vocal)<\/li>\n<li>ildefonso Armenteros armenteros (vocal)<\/li>\n<li>paul Wright (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jos\u00e9 Luis Perez Jimenez Las rocas del mioceno de la cuenca de Madrid se formaron en diferentes [&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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