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Early Paleozoic rifting and bimodal volcanism in the Ossa-Morena Zone of south-west Spain

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Abstract

Lower Paleozoic volcanic members have been investigated by geological, petrographical and geochemical means in a traverse across the Ossa-Morena Zone (OMZ) in south-west Spain.

The volcanism lasted from the Early Cambrian to the Early Ordovician, with a peak in the Middle Cambrian. The volcanism is bimodal, starting up with acidic and ending with basic compositions. From north to south, peralkaline rhyolites change to rhyolites, and strongly enriched alkali basalts change via transitional basalts to mid-ocean ridge basalt (MORB-type basalts). The geological and magmatic evolution suggests an extensive Early Paleozoic rifting with its center along the southern boundary of the OMZ. Temporal, spatial and crustal aspects of the rifting event are presented in a geodynamic model.

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Authors and Affiliations

  1. Geologisches Institut RWTH Aachen, Wüllnrierstraße 2, D-52062, Aachen, Germany

    Uwe Giese

  2. Institut für Geowissenschaften und Lithosphärenforschung, Senckenbergstr. 3, D-35390, Giessen, Germany

    Bernhard Bühn

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  1. Uwe Giese
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  2. Bernhard Bühn
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Giese, U., Bühn, B. Early Paleozoic rifting and bimodal volcanism in the Ossa-Morena Zone of south-west Spain. Geol Rundsch 83, 143–160 (1994). https://doi.org/10.1007/BF00211898

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