Paleometeorización vs. Paleoalteración en la superficie de discordancia Proterozoico-Cámbrico en el Antiforme del Narcea

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dc.contributor.authorGutiérrez Alonso, Gabriel
dc.contributor.authorBlanco Sánchez, J. A.
dc.contributor.authorMacfarlane, A.
dc.contributor.authorFernández Suárez, Javier
dc.date.accessioned2014-10-23T08:36:32Z
dc.date.available2014-10-23T08:36:32Z
dc.date.issued2004
dc.description.abstractPetrographic and geochemical characterization of the rocks underlying the Neoproterozoic-Cambrian angular unconformity in the eastern flank of the Narcea Antiform, provide an insight on the processes involved in the widespread ruhefaction present along this contact. The'data provide evidence of superposed events related to the sub-aerial weathering during the Precambrian-Cambrian boundary and a further alteration caused, probably,; by fluid circulation during the Variscan Orogenyen_US
dc.identifier.urihttp://hdl.handle.net/10272/8951
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.otherRubefactionen_US
dc.subject.otherPaleoweatheringen_US
dc.subject.otherPaleoalterationen_US
dc.subject.otherGeochemiastryen_US
dc.subject.otherCambrian-Precambrian boundaryen_US
dc.titlePaleometeorización vs. Paleoalteración en la superficie de discordancia Proterozoico-Cámbrico en el Antiforme del Narceaen_US
dc.titlePaleoweathering vs. Paleoalteration at the Proterozoic-Cambrian uncomformity surface ¡n the Narcea Antiformeng
dc.typejournal articleen_US
dspace.entity.typePublication

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Geogaceta -- Nº 36, (2004)