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Swiss Journal of Geosciences
Fig. 9 | Swiss Journal of Geosciences

Fig. 9

From: Influence of rheologically weak layers on fault architecture: insights from analogue models in the context of the Northern Alpine Foreland Basin

Fig. 9

Overview of model results from Series C, part 2: Pure dextral strike-slip along the basal fault, in model without a viscous weak layer (Model C3) and with a viscous weak layer (Model C4). Total slip is twice as much as in the pure normal dip-slip models and the 45° oblique normal slip models (i.e. 20.8 mm, after a 120 min model run)

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