Una discontinuidad estratigráfica de 6 m.a. en las calizas albienses de Aitziber (Navarra)

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dc.contributor.authorQuintanar Soto, A. B.
dc.contributor.authorFernández Mendiola, Pedro Ángel
dc.contributor.authorCaron, M.
dc.date.accessioned2015-03-30T09:45:15Z
dc.date.available2015-03-30T09:45:15Z
dc.date.issued1998
dc.description.abstractThe Aitziber calcarenites is a sedimentary unit of Upper Albian (appenninica with buxtorfi zone) age. The top of this unit records an unconformity of at least 6 m.a.. The hiatus extends from the uppermost Albian to lower Turonianen_US
dc.identifier.urihttp://hdl.handle.net/10272/10206
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherUnconformityen_US
dc.subject.otherCalcarenitesen_US
dc.subject.otherAlbian-Turonianen_US
dc.subject.otherHardgrounden_US
dc.titleUna discontinuidad estratigráfica de 6 m.a. en las calizas albienses de Aitziber (Navarra)en_US
dc.titleA 6 m.a. Stratigraphie unconformity on top of the Albian Aitziber limestones (Navarra)eng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 25, (1998)