{"id":46299,"date":"2019-10-12T21:15:15","date_gmt":"2019-10-12T21:15:15","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/estudio-sedimentologico-y-diagenetico-de-las-formaciones-carbonatadas-del-jurasico-de-los-catalanides-maestrazgo-y-rama-aragonesa-de-la-cordillera-iberica-sector-oriental\/"},"modified":"2019-10-12T21:15:15","modified_gmt":"2019-10-12T21:15:15","slug":"estudio-sedimentologico-y-diagenetico-de-las-formaciones-carbonatadas-del-jurasico-de-los-catalanides-maestrazgo-y-rama-aragonesa-de-la-cordillera-iberica-sector-oriental","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/estudio-sedimentologico-y-diagenetico-de-las-formaciones-carbonatadas-del-jurasico-de-los-catalanides-maestrazgo-y-rama-aragonesa-de-la-cordillera-iberica-sector-oriental\/","title":{"rendered":"Estudio sedimentologico y diagenetico de las formaciones carbonatadas del jurasico de los catalanides, maestrazgo y rama aragonesa de la cordillera iberica (sector oriental)."},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Giner Sanchez Jos\u00e9 A. <\/strong><\/h2>\n<p>Se establece una nueva division del jurasico en cuatro secuencias deposicionales. Lias inferior. Lias superior.  dogger y malm. Los limites entre cada secuencia corresponden a niveles ooliticos ferruginosos. Se determinan los diferentes modelos deposicionales para cada una de estas secuencias. Asimismo se interpretan las dolomitizaciones del jurasico superior como originadas por la mezcla de agua dulce y marina estableciendose el modelo correspondiente. La actividad de las fracturas tardihercinicas controlan la distribucion de las diferentes facies a lo largo del jurasico.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>Estudio sedimentologico y diagenetico de las formaciones carbonatadas del jurasico de los catalanides, maestrazgo y rama aragonesa de la cordillera iberica (sector oriental).<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 Estudio sedimentologico y diagenetico de las formaciones carbonatadas del jurasico de los catalanides, maestrazgo y rama aragonesa de la cordillera iberica (sector oriental). <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Giner Sanchez Jos\u00e9 A. <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Barcelona<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 01\/01\/1980<\/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>Mateo Esteban Cerda<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Salvador Reguant Serra <\/li>\n<li> Fontbote Mussolas Jos\u00e9 Mar\u00eda (vocal)<\/li>\n<li> San Miguel Arribas Alfredo (vocal)<\/li>\n<li>Oriol Riba Arderiu (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Giner Sanchez Jos\u00e9 A. Se establece una nueva division del jurasico en cuatro secuencias deposicionales. Lias inferior. [&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 center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-gradient":""}},"footnotes":""},"categories":[951,27,953,5040],"tags":[109995,110998,110999,80,19689,235],"class_list":["post-46299","post","type-post","status-publish","format-standard","hentry","category-barcelona","category-ciencias-de-la-tierra-y-del-espacio","category-geologia","category-geologia-del-petroleo","tag-fontbote-mussolas-jose-maria","tag-giner-sanchez-jose-a","tag-mateo-esteban-cerda","tag-oriol-riba-arderiu","tag-salvador-reguant-serra","tag-san-miguel-arribas-alfredo"],"_links":{"self":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/46299","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/comments?post=46299"}],"version-history":[{"count":0,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/posts\/46299\/revisions"}],"wp:attachment":[{"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/media?parent=46299"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/categories?post=46299"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.deberes.net\/tesis\/wp-json\/wp\/v2\/tags?post=46299"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}