RT Journal Article
T1 Mega-debris flows en el tránsito Devónico-Carbonífero de la Faja Pirítica Ibérica
T1 Mega-debris flows in the Devonian-Carboniferous boundary of the Iberian Pyrite Belt
A1 Moreno Garrido, María Carmen
A1 Sierra del Pino, Sonia
A1 Sáez Ramos, Reinaldo
AB 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
PB Sociedad Geológica de España
YR 1994
FD 1994
LK http://hdl.handle.net/10272/13792
UL http://hdl.handle.net/10272/13792
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026