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The paleokarstic structures of Monte Baio (Araba/Alava): their relevance for a quantitative évaluation of the mid-Paleocene sea-level fall

dc.contributor.authorBaceta, Juan Ignacio
dc.contributor.authorPujalte, Victoriano
dc.contributor.authorPayros, Aitor
dc.date.accessioned2015-05-13T08:00:02Z
dc.date.available2015-05-13T08:00:02Z
dc.date.issued1997
dc.identifier.urihttp://hdl.handle.net/10272/10589
dc.description.abstractDuring the period of sub-aerial exposure subsequent to the mid-Paleocene sea level fall, a set of paleokarstic features were generated in upper Danian lagoonal limestones of the Alava province. The most interesting of them all, and potentially the more meaningful, is a horizontal dissolution horizon, possibly recording the position of the upper surface of a paleophreatic zone. If that possibility is correct, the magnitude of the mid-Paleocene sea level fall would be narrowly constrained to circa 40 m/a more realistic figure than those previously estimated for this eventen_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.otherPaleokarsten_US
dc.subject.otherMid-Paleoceneen_US
dc.subject.otherSea-level fallen_US
dc.subject.otherSouthern Pyreneesen_US
dc.subject.otherAraba/Alavaen_US
dc.titleLas estructuras paleokársticas del Monte Baio (Araba/Alava): su relevancia para una evaluación cuantitativa del descenso del nivel marino del Paleoceno medioen_US
dc.titleThe paleokarstic structures of Monte Baio (Araba/Alava): their relevance for a quantitative évaluation of the mid-Paleocene sea-level falleng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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