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Swiss Journal of Geosciences
Fig. 8 | Swiss Journal of Geosciences

Fig. 8

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

Fig. 8

Overview of model results from Series C, part 1: 45° (dextral) oblique normal slip along the basal fault, without a detachment in Model C1, and with a full viscous detachment in Model C2. 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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