RT Journal Article
T1 La transición de pliegues de despegue a pliegues de propagación: el ejemplo del anticlinal de Aguilón (Cordillera Ibérica)
T1 On the transition from detachment folds to fault-propagation folds: example from the Aguilon anticline (Iberian Chain)
A1 Cortés Gracia, A. L.
A1 Casas Sainz, Antonio
AB The northern border of the Iberian Chain shows detachment and fault-propagation folds that deform the mesozoic and tertiary sedimerits near Zaragoza. The regional detachment level are the lutitic and gypsyferous beds of the Upper Triassic. The thickness of the cover and the detachment level determine the kinematic evolution of folds that show intermediate geometry between detachment and faultpropagation types
PB Sociedad Geológica de España
YR 1995
FD 1995
LK http://hdl.handle.net/10272/13418
UL http://hdl.handle.net/10272/13418
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 31 may 2026