@article{10272/12207,
year = {1996},
url = {http://hdl.handle.net/10272/12207},
abstract = {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},
publisher = {Sociedad Geológica de España},
title = {Relaciones entre la evolución sedimentaria del Grupo de Arén y el Cabalgamiento de Boixols (Campaniense terminalMaastrichtiense del Pirineo Meridional -Central)},
title = {Relations between the sedimentary evolution of the Aren Group and the Boixols thrust (Uppermost CampanianMaastrichtian of South-Central Pyrenees)},
author = {Arbués, Pelayo and Pi, E. and Berástegui, X.},
}