Paleometeorización vs. Paleoalteración en la superficie de discordancia Proterozoico-Cámbrico en el Antiforme del Narcea
2004; Issue: 36 Linguagem: Inglês
ISSN
2173-6545
AutoresGabriel Gutiérrez‐Alonso, José Antonio Blanco Sánchez, A. Macfarlane, Javier Fernández‐Suárez,
Tópico(s)Archaeological and Historical Studies
ResumoPetrographic 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 involvedin the widespread rubefaction present along this contacto The data provide evidence of superposed events related to the sub-aerial weathering during the Precambria-Cambrian boundary and a further alteration caused, probably by fluid circulation during the Variscan Orogeny.
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