A late Fammenian age storm-dominated succession at Berrocal (Iberian Pyrite Belt - Spain)

Fernandes, Paulo; Pereira, Zélia; Oliveira, José Tomás; Jorge, R. C. G. S.; Relvas, J.

http://hdl.handle.net/10400.1/5066

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Abstract(s)

The Berrocal area is situated in the northern limb of Valverde del Camino anticlinal in the Spanish sector the Iberian Belt and exposes the upper part of the Phyllite-Quartzite Group. Recent studies on palynostratigraphy and sedimentology of the Berocal section indicates that the stratigraphic succession is late Famennian age (VH miospore biozone) and was accumulated on the offshore zone of a siliciclastic shelf dominated by storm events.

Keywords

Late Famennian Palynomorphs Tempestites Pyrite Belt South Portuguese Zone

URI

http://hdl.handle.net/10400.1/5066

Citation

Fernandes, Paulo; Pereira, Zélia; Oliveira, José Tomás; Jorge, R.C.G.S.; Jorge Relvas. A Late Fammenian age storm-dominated succession at Berrocal (Iberian Pyrite Belt - Spain), Trabalho apresentado em CIMP Lisbon´7, Joint Meeting of Spores/Pollen and Acritarch Subcommissions, In CIMP Lisbon´7, Joint Meeting of Spores/Pollen and Acritarch Subcommissions, Lisboa, 2007.