Mega-debris flows en el tránsito Devónico-Carbonífero de la Faja Pirítica Ibérica
Loading...
Publication date
Advisors
Department
Research group
Center
Metrics
Export
Abstract
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
Keywords
Unesco Subjects
Bibliographic citation
Collections
The license for this item is described as Atribución-NoComercial-SinDerivadas 3.0 España