{"id":52568,"date":"2022-03-22T05:31:01","date_gmt":"2022-03-22T05:31:01","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/sedimentologia-y-diagenesis-del-buntsandstein-y-muschel-kalk-de-la-rama-aragonesa-de-la-cordillera-iberica-provincias-de-soria-y-zaragoza\/"},"modified":"2022-03-22T05:31:01","modified_gmt":"2022-03-22T05:31:01","slug":"sedimentologia-y-diagenesis-del-buntsandstein-y-muschel-kalk-de-la-rama-aragonesa-de-la-cordillera-iberica-provincias-de-soria-y-zaragoza","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/sedimentologia-y-diagenesis-del-buntsandstein-y-muschel-kalk-de-la-rama-aragonesa-de-la-cordillera-iberica-provincias-de-soria-y-zaragoza\/","title":{"rendered":"Sedimentolog\u00eda y diagenesis del buntsandstein y muschel kalk de la rama aragonesa de la cordillera iberica (provincias de soria y zaragoza)."},"content":{"rendered":"<h2>Tesis doctoral de <strong> Jose Arribas Mocoroa <\/strong><\/h2>\n<p>Se han definido distintas unidades litoestratigraficas informales sobre las que se realiza el analisis de facies y su interpretacion sedimentologica. Asimismo se caracterizan petrologicamente los depositos detriticos tanto textual como composicionalmente  realizandose un estudio de su procedencia. Por ultimo se desarrollan los procesos diageneticos sufridos en las areniscas  haciendo hincapie en la compactacion  origen de la matriz cementacion  reemplazamientos y alteraciones  y porosidad. El analisis de las facies carbonaticas pasa por el estudio de sus microfacies asi como de sus secuencias para poder realizar su interpretacion sedimentologica. Dentro de los procesos postsedimentarios se aborda el tema de la dolomitizacion  dedolomitizacion y silicificacion.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Sedimentolog\u00eda y diagenesis del buntsandstein y muschel kalk de la rama aragonesa de la cordillera iberica (provincias de soria y zaragoza).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Sedimentolog\u00eda y diagenesis del buntsandstein y muschel kalk de la rama aragonesa de la cordillera iberica (provincias de soria y zaragoza). <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Jose Arribas Mocoroa <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Complutense de Madrid<\/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> Pe\u00f1a Blasco Jos\u00e9 Andr\u00e9s De La<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Carmina Virgili Rodon <\/li>\n<li>Rafaela Marfil Perez (vocal)<\/li>\n<li>Juan Rosell Sanvy (vocal)<\/li>\n<li>Federico Orti Cabo (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Jose Arribas Mocoroa Se han definido distintas unidades litoestratigraficas informales sobre las que se realiza el analisis [&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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