RT Journal Article
T1 Relaciones entre la evolución sedimentaria del Grupo de Arén y el Cabalgamiento de Boixols (Campaniense terminalMaastrichtiense del Pirineo Meridional -Central)
T1 Relations between the sedimentary evolution of the Aren Group and the Boixols thrust (Uppermost CampanianMaastrichtian of South-Central Pyrenees)
A1 Arbués, Pelayo
A1 Pi, E.
A1 Berástegui, X.
AB The Arén Croup was deposited synchronously to the growth of the Boixols thrust. Sedimentation took place in siliciclastic marine and alluvial environments. The growth of a footwall syncline affected the geometry of the basin fill by adding drowning and uplifting movements. Such a mechanism might be common to those settings where fault propagation folds develop. In the Arén Croup, this differential subsidence mechanism was not able to overprint the identified sedimentary cycles
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/12207
UL http://hdl.handle.net/10272/12207
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026