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Swiss Journal of Geosciences
Fig. 10 | Swiss Journal of Geosciences

Fig. 10

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

Fig. 10

Overview of model results from Series D, part 1: Pure normal dip-slip along the basal fault, with a kinetic sand layer in Model D1, and with a weak viscous layer in Model D2. Max./Min. NS (incr.): Incremental maximum/minimum normal strain, indicating extension or contraction in the model, respectively. Vy: incremental displacement in the y-direction. Note that section locations are not indicated due to the progressive sectioning method (see Sect. 3.5 and Fig. 4)

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