Mega-debris flows en el tránsito Devónico-Carbonífero de la Faja Pirítica Ibérica.

• Autores: María Carmen Moreno Garrido, Sonia Sierra del Pino, Reinaldo Sáez Ramos
• Localización: Geogaceta, ISSN 0213-683X, Nº. 17, 1994, págs. 9-11
• Idioma: español
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• Resumen

  • Detrital platform sedimentation during the Devonian times took place in the homogeneous basin of the Iberian Pyrite Belt. This shallow basin changed to a mosaic of horsts and grabens just in the Devonian-Carboniferous boundary. Thick mattrix supported conglomerates (mega-debris flow) appear related with this dynamic. They suggest convulsive seismic events related to the Breton phase of the Hercynian orogeny