Mega-debris flows en el tránsito Devónico-Carbonífero de la Faja Pirítica Ibérica.
- Moreno Garrido, María Carmen
- Sierra del Pino, Sonia
- Sáez Ramos, Reinaldo
ISSN: 0213-683X
Datum der Publikation: 1994
Nummer: 17
Seiten: 9-11
Art: Artikel
Andere Publikationen in: Geogaceta
Zusammenfassung
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