{"id":49737,"date":"2021-05-07T06:03:53","date_gmt":"2021-05-07T06:03:53","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-y-sedimentologia-del-paleogeno-en-el-borde-suroccidental-de-la-cuenca-del-duero-provincia-de-salamanca\/"},"modified":"2021-05-07T06:03:53","modified_gmt":"2021-05-07T06:03:53","slug":"estratigrafia-y-sedimentologia-del-paleogeno-en-el-borde-suroccidental-de-la-cuenca-del-duero-provincia-de-salamanca","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-y-sedimentologia-del-paleogeno-en-el-borde-suroccidental-de-la-cuenca-del-duero-provincia-de-salamanca\/","title":{"rendered":"Estratigrafia y sedimentolog\u00eda del paleogeno en el borde suroccidental de la cuenca del duero (provincia de salamanca)"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Gaspar Alonso Gavilan <\/strong><\/h2>\n<p>Se establece la serie general del paleogeno de dicho borde  definiendose cuatro formaciones como constituyentes principales. Del estudio de estas formaciones se obtienen las caracteristicas sedimentologicas       en funcion de la asociacion de f acies que presentan  y se deduce el medio deposicional para cada unidad. Teniendo en cuenta los resultados obtenidos en este estudio  se ha reconstruido la historia geologica que acontecio en este borde de la cuenca del duero durante el paleogeno<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia y sedimentolog\u00eda del paleogeno en el borde suroccidental de la cuenca del duero (provincia de salamanca)<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia y sedimentolog\u00eda del paleogeno en el borde suroccidental de la cuenca del duero (provincia de salamanca) <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Gaspar Alonso Gavilan <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Salamanca<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1982<\/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>Inmaculada Corrales Zarauza<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carlos Garcia Figuerola <\/li>\n<li>Inmaculada Corrales Zarauza (vocal)<\/li>\n<li>Juan Rosell Sanuy (vocal)<\/li>\n<li> Valladares Gonzalez Mar\u00eda  Isabel (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gaspar Alonso Gavilan Se establece la serie general del paleogeno de dicho borde definiendose cuatro formaciones como [&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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