Fig. 11From: Influence of rheologically weak layers on fault architecture: insights from analogue models in the context of the Northern Alpine Foreland BasinOverview of model results from Series D, part 2 (Model D3): Pure dextral fast strike-slip along the basal fault with a full viscous layer. Total fault 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)Back to article page