{"id":24908,"date":"2018-03-09T09:16:04","date_gmt":"2018-03-09T09:16:04","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-cretacico-medio-del-extremo-suroriental-del-anticlinorio-de-bilbao-estratigrafia-y-sedimentologa%c2%ada\/"},"modified":"2018-03-09T09:16:04","modified_gmt":"2018-03-09T09:16:04","slug":"el-cretacico-medio-del-extremo-suroriental-del-anticlinorio-de-bilbao-estratigrafia-y-sedimentologa%c2%ada","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/pais-vasco-euskal-herriko-unibertsitatea\/el-cretacico-medio-del-extremo-suroriental-del-anticlinorio-de-bilbao-estratigrafia-y-sedimentologa%c2%ada\/","title":{"rendered":"El cret\u00e1cico medio del extremo suroriental del anticlinorio de bilbao: estratigrafia y sedimentolog\u00eda"},"content":{"rendered":"<h2>Tesis doctoral de <strong>  Quintanar Soto Ana Bel\u00e9n <\/strong><\/h2>\n<p>Esta memoria aporta una cartograf\u00eda novedosa 1:25000 del extremo suroriental del anticlinorio de bilbao, en la zona de alsasua. Se han realizado adem\u00e1s cartograf\u00edas de detalle (1:10000) de las plataformas carbonatadas estudiadas.  en el cap\u00edtulo de estratigraf\u00eda se definen tres formaciones (eguino, araya y aitziber), y una unidad estratigr\u00e1fica informal (elkuden), y se citan por primera vez en la zona una especie de ammonite (extremo techo del albiense medio) y varias especies de foramin\u00edferos planct\u00f3nicos (albiense superior (zona inflatum-santoniense). Sedimentol\u00f3gicamente se describen tres sistemas deposicionales: plataforma carbonatada-talud-cuenca de eguino, rampa carbonatada de aitziber y cuenca de elkuden-araya-olazagutia, que se organizan secuencialmente en tres megasecuencias:  1,- albiense superior, zona inflatum  2,- albiense superior, zona dispar  3,- cenomaniense inferior, zonas globotruncanoides-reicheli  en el apartado de tect\u00f3nica se describen fallas sinsedimentarias que actuaron durante dos etapas de tect\u00f3nica sinsedimenteria, la primera etapa durante el albiense superior (zona inflatum) y la segunda en el albiense superior (zona dispar), \u00e9stas dos etapas configuraron sendas paleogeograf\u00edas, todo ello contextualizado dentro de la apertura de la cuenca vasco cant\u00e1brica y la deriva de iberia.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El cret\u00e1cico medio del extremo suroriental del anticlinorio de bilbao: estratigrafia y sedimentolog\u00eda<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El cret\u00e1cico medio del extremo suroriental del anticlinorio de bilbao: estratigrafia y sedimentolog\u00eda <\/li>\n<li><strong>Autor:<\/strong>\u00a0  Quintanar Soto Ana Bel\u00e9n <\/li>\n<li><strong>Universidad:<\/strong>\u00a0 Pa\u00eds vasco\/euskal herriko unibertsitatea<\/li>\n<li><strong>Fecha de lectura de la tesis:<\/strong>\u00a0 18\/07\/2003<\/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>Pedro Angel Fernandez Mendiola<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: joaqu\u00edn Garc\u00eda mond\u00e9jar <\/li>\n<li> Bahamonde rionda Juan  ram\u00f3n (vocal)<\/li>\n<li>arantza Aranburu artano (vocal)<\/li>\n<li>Alberto P\u00e9rez l\u00f3pez (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Quintanar Soto Ana Bel\u00e9n Esta memoria aporta una cartograf\u00eda novedosa 1:25000 del extremo suroriental del anticlinorio de [&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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