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Fig. 13 | Swiss Journal of Geosciences

Fig. 13

From: 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)

Fig. 13

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)

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