{"id":39792,"date":"1999-01-01T00:00:00","date_gmt":"1999-01-01T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/analisis-de-los-sistemas-deposicionales-carbonaticos-y-evaporiticos-del-neogeno-de-la-cuenca-de-calatayud-provincia-de-zaragoza\/"},"modified":"1999-01-01T00:00:00","modified_gmt":"1999-01-01T00:00:00","slug":"analisis-de-los-sistemas-deposicionales-carbonaticos-y-evaporiticos-del-neogeno-de-la-cuenca-de-calatayud-provincia-de-zaragoza","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/analisis-de-los-sistemas-deposicionales-carbonaticos-y-evaporiticos-del-neogeno-de-la-cuenca-de-calatayud-provincia-de-zaragoza\/","title":{"rendered":"Analisis de los sistemas deposicionales carbonaticos y evaporiticos del neogeno de la cuenca de calatayud (provincia de zaragoza)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Enrique Sanz Rubio <\/strong><\/h2>\n<p>En el registro sedimentario ne\u00f3geno de la cuenca de calatayud se han diferenciado tres unidades mayores denominadas unidad inferior, intermedia y superior. Las unidades inferior e intermedia poseen un car\u00e1cter evapor\u00edtico mientras que la unidad superior responde a un sistema fluvio-lacuestre carbon\u00e1tico de agua dulce. La unidad intermedia se caracteriza por una gran complejidad; su arquitectura deposicional responde a la g\u00e9nesis de un paleorrelieve a techo de la unidad inferior, ligado a karstificaci\u00f3n de yesos. Adem\u00e1s, registra grandes cuerpos formados por carbonatos diagen\u00e9ticos (calcita) que se encuentran influenciados por un cambio en la hidroqu\u00edmica de las aguas de la cuenca.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Analisis de los sistemas deposicionales carbonaticos y evaporiticos del neogeno de la cuenca de calatayud (provincia de zaragoza).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Analisis de los sistemas deposicionales carbonaticos y evaporiticos del neogeno de la cuenca de calatayud (provincia de zaragoza). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Enrique Sanz Rubio <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1999<\/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>Manuel Hoyos Gomez<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: cristino jose Dabrio gonzalez <\/li>\n<li>salvador Ordo\u00f1ez delgado (vocal)<\/li>\n<li>jean marie Rouchy (vocal)<\/li>\n<li> Garcia del cura m. angeles (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Enrique Sanz Rubio En el registro sedimentario ne\u00f3geno de la cuenca de calatayud se han diferenciado tres [&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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