{"id":46004,"date":"2019-08-24T05:34:15","date_gmt":"2019-08-24T05:34:15","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estratigrafia-y-sedimentologia-de-las-formaciones-detriticas-del-cretacico-inferior-terminal-en-el-bajo-aragon-turolense\/"},"modified":"2019-08-24T05:34:15","modified_gmt":"2019-08-24T05:34:15","slug":"estratigrafia-y-sedimentologia-de-las-formaciones-detriticas-del-cretacico-inferior-terminal-en-el-bajo-aragon-turolense","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estratigrafia-y-sedimentologia-de-las-formaciones-detriticas-del-cretacico-inferior-terminal-en-el-bajo-aragon-turolense\/","title":{"rendered":"Estratigrafia y sedimentolog\u00eda de las formaciones detriticas del cretacico inferior terminal en el bajo aragon turolense"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Gonzalo Pardo Tirapu <\/strong><\/h2>\n<p>Se realiza un estudio estratigrafico y sedimentologico de las formaciones escucha y utrillas en el n. De la provincia de teruel  estableciendose sus limites y la division en miembros de la fm. Escucha. Se pone de manifiesto que la fm. Escucha corresponde a la progradacion de un medio deltaico s.L.  Donde se reconoce la sucesion vertical y horizontal de subambientes mareales  palustres y fluviales. La fm. Utrillas correspondiente al comienzo de un ciclo transgresivo  se inicia sobre una disconformidad  evolucionando desde un medio fluvial a medios transicionales con los que se realiza el paso a la sedimentacion calcarea del cretacico superior.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estratigrafia y sedimentolog\u00eda de las formaciones detriticas del cretacico inferior terminal en el bajo aragon turolense<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estratigrafia y sedimentolog\u00eda de las formaciones detriticas del cretacico inferior terminal en el bajo aragon turolense <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Gonzalo Pardo Tirapu <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Zaragoza<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1979<\/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>Joaquin Villena Morales<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Oriol Riba Arderiu <\/li>\n<li> Sanchez De La Torre Luis (vocal)<\/li>\n<li>Felix Arrese Serrano (vocal)<\/li>\n<li>Inmaculada Corrales Zarauza (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Gonzalo Pardo Tirapu Se realiza un estudio estratigrafico y sedimentologico de las formaciones escucha y utrillas en [&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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