@article{10272/8273,
year = {2008},
url = {http://hdl.handle.net/10272/8273},
abstract = {Paleogene rocks crop out in the South Pyrenean Zone as a flysch sequence of calcarenites and mudstones
showing asymmetric south-verging chevron folds, with associated axial plane foliation. Thrust faults are
generated at the long limbs of the chevron folds. They have duplex type geometry and, in particular,
geometric features similar to those that characterize flexural slip duplexes. These show planar or gently
curved roof and floor thrusts and the absence of ramp anticlines. The hanging-wall shows southwards
sense of movement, which is in agreement with the vergence of other structures in the work area.
Because pinnate joints related to thrusts planes cut clearly the axial plane foliation, thrusts are generated
later than angular folds},
keywords = {Thrusts},
keywords = {Chevron folds},
keywords = {South Pyrenean Zone},
title = {Geometría de cabalgamientos asociados a flancos normales de pliegues (N de Biescas, Zona Surpirenaica)},
title = {Geometry of thrusting related to normal limbs of chevron folds (North of Biescas, South Pyrenean Zone)},
author = {Rodríguez, Lidia and Cuevas, Julia},
}