{"id":71164,"date":"2004-10-11T00:00:00","date_gmt":"2004-10-11T00:00:00","guid":{"rendered":"https:\/\/www.deberes.net\/tesis\/sin-categoria\/la-depresion-intermedia-entre-leitzia-y-elizondo-pirineo-occidental-estratigrafa%c2%ada-y-relaciones-tectonica\/"},"modified":"2004-10-11T00:00:00","modified_gmt":"2004-10-11T00:00:00","slug":"la-depresion-intermedia-entre-leitzia-y-elizondo-pirineo-occidental-estratigrafa%c2%ada-y-relaciones-tectonica","status":"publish","type":"post","link":"https:\/\/www.deberes.net\/tesis\/ciencias-de-la-tierra-y-del-espacio\/la-depresion-intermedia-entre-leitzia-y-elizondo-pirineo-occidental-estratigrafa%c2%ada-y-relaciones-tectonica\/","title":{"rendered":"La depresi\u00f3n intermedia entre leitzia y elizondo (pirineo occidental); estratigraf\u00eday relaciones tect\u00f3nica"},"content":{"rendered":"<h2>Tesis doctoral de <strong> Eneko Iriarte Avil\u00e9s <\/strong><\/h2>\n<p>Se presentan los resultados del estudio del cret\u00e1cico de la parte oriental de la depresi\u00f3n intermedia, entre las localidades de leitza y el\u00edzondo (pirineos occidentales, navarra). Para la informaci\u00f3n b\u00e1sica se han elaborado cartograf\u00edas a escala 1:25.000, y localmente, a 1:10.000. Se han diferenciado 6 unidades y 5 subunidades litoestratigr\u00e1fica in\u00e9ditas, las cuales han sido caracterizadas bioestrateigr\u00e1ficamente mediante foramin\u00edferos bent\u00f3nicos (calizas del apti\u00e9nse-albiense) y foramin\u00edferos planct\u00f3nicos (margas y calizas del cenomaniense-santoniense).  se han definido 4 asociaciones de foramin\u00edferos planct\u00f3nicos, correspondientes al albiense superior-cenomaniense inferior. Turoniense superior, turoniense superior-coniaciense y santoniense.  se propone la creaci\u00f3n de una nueva biozonal local, zona falsotruncana maslakovae, para el turoniense superior. La dataci\u00f3n precisa de materiales ha permitido distinguir lagunas estratigr\u00e1ficas, entre las que destacan una de albiense medio y otra entre el albiense superior final (vraconiense) y el turoniense superior.  sedmientol\u00f3gicamente se han distinguido 3 sistemas deposionales:  1, plataforma carbonatada de mokorro (aptiense superior-albiense inferior).  2, plataforma mixta-talud-cuenca de aixterri (albiense superior-cenomaniense inferior).  3, plataforma-cuenca carbonatada de galardea (turoniense superior-campaniense).  varios sistemas de fallas, pliegues, discordancias, surcos y subcuencas se consideran sinsedimentarias.  se agrupan en 5 frases tectosedimentarias:  fase i: aptiense superior-albiense inferior.  fase ii: albiense medio-albiense superior basal.  fase iii: albiense superior.  fase iv: albiense superior final (vraconiense)-cenomaniense inferior.  fase v: turoniense superior-coniaciense.  denonatan la existencia continuada de un r\u00e9gimen de esfuerzos transtensivo senestro, excepto en la fase iv (alb\u00edense superior-vraconiense), compatible con es<\/p>\n<p>&nbsp;<\/p>\n<h3>Datos acad\u00e9micos de la tesis doctoral \u00ab<strong>La depresi\u00f3n intermedia entre leitzia y elizondo (pirineo occidental); estratigraf\u00eday relaciones tect\u00f3nica<\/strong>\u00ab<\/h3>\n<ul>\n<li><strong>T\u00edtulo de la tesis:<\/strong>\u00a0 La depresi\u00f3n intermedia entre leitzia y elizondo (pirineo occidental); estratigraf\u00eday relaciones tect\u00f3nica <\/li>\n<li><strong>Autor:<\/strong>\u00a0 Eneko Iriarte Avil\u00e9s <\/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 10\/11\/2004<\/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 Garc\u00eda Mond\u00e9jar<\/li>\n<\/ul>\n<\/li>\n<li><strong>Tribunal<\/strong>\n<ul>\n<li>Presidente del tribunal: cristino jose Dabrio gonzalez <\/li>\n<li>ram\u00f3n Salas roig (vocal)<\/li>\n<li>arantza Aranburu artano (vocal)<\/li>\n<li>pedro angel Fernandez mendiola (vocal)<\/li>\n<\/ul>\n<\/li>\n<\/ul>\n<p>&nbsp;<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Tesis doctoral de Eneko Iriarte Avil\u00e9s Se presentan los resultados del estudio del cret\u00e1cico de la parte oriental de la 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