Gutiérrez Alonso, GabrielBlanco Sánchez, J. A.Macfarlane, A.Fernández Suárez, Javier2014-10-232014-10-232004http://hdl.handle.net/10272/8951Petrographic 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 OrogenyspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/RubefactionPaleoweatheringPaleoalterationGeochemiastryCambrian-Precambrian boundaryPaleometeorización vs. Paleoalteración en la superficie de discordancia Proterozoico-Cámbrico en el Antiforme del NarceaPaleoweathering vs. Paleoalteration at the Proterozoic-Cambrian uncomformity surface ¡n the Narcea Antiformjournal articleopen access