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

  1. Moreno Garrido, María Carmen
  2. Sierra del Pino, Sonia
  3. Sáez Ramos, Reinaldo
Revista:
Geogaceta

ISSN: 0213-683X

Año de publicación: 1994

Número: 17

Páginas: 9-11

Tipo: Artículo

DIALNET GOOGLE SCHOLAR lock_openArias Montano editor

Otras publicaciones en: Geogaceta

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

Fuente de los datos: Dialnet