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Stratigraphic significance of two alterations in the Late Miocene of the Duero Basin

dc.contributor.authorArmenteros, Ildefonso
dc.date.accessioned2020-05-27T08:39:55Z
dc.date.available2020-05-27T08:39:55Z
dc.date.issued1991
dc.identifier.urihttp://hdl.handle.net/10272/18085
dc.description.abstractAnalysis was made of two alterations located within and on the top of the Late Miocene in the central-eastern region of the Duero Basin. Questions arising about their stratigraphic significance are a/so approached. The Iower alteration affects the top of marly-gypsiferous unit (U. 3) and is related to major paleogeographic change towards less evaporitic conditions. The upper alteration defines the upper boundary of Neogene record in the basin and is related to the extensive Plio-Pleistocene pediment, which bevels the Neogene serie from the borders to the centre of the basines_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherAlterationes_ES
dc.subject.otherDiscontinutyes_ES
dc.subject.otherLate Miocenees_ES
dc.subject.otherTertiary Duero Basines_ES
dc.subject.otherSpaines_ES
dc.titleSignificado estratigráfico de dos alteraciones en el Mioceno superior de la Cuenca del Dueroes_ES
dc.titleStratigraphic significance of two alterations in the Late Miocene of the Duero Basineng
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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