@article{10272/13792,
year = {1994},
url = {http://hdl.handle.net/10272/13792},
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},
publisher = {Sociedad Geológica de España},
title = {Mega-debris flows en el tránsito Devónico-Carbonífero de la Faja Pirítica Ibérica},
title = {Mega-debris flows in the Devonian-Carboniferous boundary of the Iberian Pyrite Belt},
author = {Moreno Garrido, María Carmen and Sierra del Pino, Sonia and Sáez Ramos, Reinaldo},
}