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A Bartonian channel-levee turbidite sys tem in the Pamplona Basin: tectonic and paleogeographic implications

dc.contributor.authorPayros, Aitor
dc.contributor.authorPujalte, Victoriano
dc.contributor.authorOrue Etxebarria, Xabier
dc.contributor.authorBaceta, Juan Ignacio
dc.date.accessioned2015-05-13T11:15:13Z
dc.date.available2015-05-13T11:15:13Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10604
dc.description.abstractThe Bartonian Ezkaba Sandstone, in the Pamplona Basin,.seems.to represent channel-fill deposits of a laterally migrating ch.annel-levee turbidite.system. Its silicidastic nature and its northern derivation indicate the contemporaneous emergence of the orogenic inner zones .in the western Pyreneesen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherEocene/ western Pyreneesen_US
dc.subject.otherChannel-levee turbidite systemen_US
dc.subject.otherOrogenic implicationsen_US
dc.titleUn sistema turbidítico Bartoniense de tipo «channel-levee» en la Cuenca de Pamplona: implicaciones tectónicas y paleogeográficasen_US
dc.titleA Bartonian channel-levee turbidite sys tem in the Pamplona Basin: tectonic and paleogeographic implicationseng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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