{"id":52377,"date":"2022-02-19T04:47:54","date_gmt":"2022-02-19T04:47:54","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/evolucion-ambiental-y-diagenetica-de-los-depositos-del-terciario-inferior-paleoceno-y-eoceno-de-la-cuenca-de-vic\/"},"modified":"2022-02-19T04:47:54","modified_gmt":"2022-02-19T04:47:54","slug":"evolucion-ambiental-y-diagenetica-de-los-depositos-del-terciario-inferior-paleoceno-y-eoceno-de-la-cuenca-de-vic","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/evolucion-ambiental-y-diagenetica-de-los-depositos-del-terciario-inferior-paleoceno-y-eoceno-de-la-cuenca-de-vic\/","title":{"rendered":"Evolucion ambiental y diagenetica de los depositos del terciario inferior (paleoceno y eoceno) de la cuenca de vic."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Concepci\u00f3n Taberner Hern\u00e1ndez <\/strong><\/h2>\n<p>En este trabajo se analizan las caracteristicas sedimentologicas  petrologicas y diageneticas del conjunto de depositos del paleoceno y eoceno que rellenaron un area de sedimentacion diferenciada dentro de la cuenca terciaria catalana: cuenca de vic. Se han diferenciado tres tipos de depositos: terrigenos ( alluvial -fan    fan &#8211; delta   playas  deltas  y turbiditas someras)  carbonaticos (plataformas arrecifales y en rampa)  y evaporitas. Estos depositos rellenaron un sistema de surcos y umbrales tectonicamente activos hasta el eoceno medio. Como colmatacion final de la cuenca  y tras un importante cambio eustatico  se desarrollaron las evaporitas. El cambio en la sedimentacion representado por la deposicion evaporitica puede correlacionarse con el llamado evento del eoceno terminal.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Evolucion ambiental y diagenetica de los depositos del terciario inferior (paleoceno y eoceno) de la cuenca de vic.<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Evolucion ambiental y diagenetica de los depositos del terciario inferior (paleoceno y eoceno) de la cuenca de vic. <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Concepci\u00f3n Taberner Hern\u00e1ndez <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1984<\/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> San Miguel Arribas Alfredo<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Salvador Reguant Serra <\/li>\n<li>Oriol Riba Arderiu (vocal)<\/li>\n<li> San Miguel Arribas  Alfredo (vocal)<\/li>\n<li> Porta Vernet  Jaime De (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Concepci\u00f3n Taberner Hern\u00e1ndez En este trabajo se analizan las caracteristicas sedimentologicas petrologicas y diageneticas del conjunto de [&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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