{"id":44858,"date":"2019-01-16T00:30:46","date_gmt":"2019-01-16T00:30:46","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/el-complejo-purbeck-weald-de-santander-estratigrafia-y-sedimentacion\/"},"modified":"2019-01-16T00:30:46","modified_gmt":"2019-01-16T00:30:46","slug":"el-complejo-purbeck-weald-de-santander-estratigrafia-y-sedimentacion","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/el-complejo-purbeck-weald-de-santander-estratigrafia-y-sedimentacion\/","title":{"rendered":"El complejo purbeck-weald de santander: estratigrafia y sedimentacion"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Victoriano Pujalte Navarro <\/strong><\/h2>\n<p>El complejo purbeck-weald de santander tiene un espesor no inferior a 2.000 m en santander. La sucesion descansa sobre una superficie erosiva  encima de sedimentos carbonatados marinos de calloviense inf  y termina con el advenimiento de los estratos urfonianos en el aptiense inf. Se reconocen dos ciclos sedimentarios mayores y el comienzo de un tercero. Cada ciclo  que sucede a una discontinuidad estratigrafica importante  comienza con un intervalo clastico de grano grueso que grada  hacia arriba  a sedimentos mas finos  y carbonatos  de diferentes tipos de sedimentacion. La sucesion se acumulo en una cuenca alargada e-w y fallada. Los materiales clasticos proceden de ares situadas al w y s  y la cuenca tuvo conexiones con el mar por el e y n. El desarrollo e historia de la cuenca estuvo controlado por la reactivacion de fallas tardihercinicas. La velocidad de los procesos de fallado cambio marcadamente  conduciendo asi a la constitucion de los sucesivos mefaciclotomas.<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>El complejo purbeck-weald de santander: estratigrafia y sedimentacion<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 El complejo purbeck-weald de santander: estratigrafia y sedimentacion <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Victoriano Pujalte Navarro <\/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 01\/01\/1978<\/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>Victor Garcia Due\u00f1as<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: Percibal Allen <\/li>\n<li>Antonio Cendrero (vocal)<\/li>\n<li>Juan Rossell Sanuy (vocal)<\/li>\n<li>Jos\u00e9 Mar\u00eda Amigo Descarrega (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Victoriano Pujalte Navarro El complejo purbeck-weald de santander tiene un espesor no inferior a 2.000 m 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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