Fig. 13From: Mimicking Alpine thrusts by passive deformation of synsedimentary normal faults: a record of the Jurassic extension of the European margin (Mont Fort nappe, Pennine Alps)Conceptual model of passive deformation of a pre-existing discordance. a Initial geometry resulting from the movement of a high-angle synsedimentary normal fault. b Transformation of the initial geometry by heterogeneous simple shear (sinusoidal function). Modeling was performed using the Shear2F software (Rey 2002)Back to article page