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Swiss Journal of Geosciences
Fig. 14 | Swiss Journal of Geosciences

Fig. 14

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

Fig. 14

Comparison of seismically mapped structures in the Zürcher Weinland region (compare Fig. 1b for location) redrawn in 3D after Roche et al. (2020) and our analogue model results. Middle: Structural map at Top Muschelkalk level, i.e. the top of the brittle sequence underlying the Opalinus Clay. a–d 3D sketches of the natural examples and respective analogue models from this study. a, b comparison of the Rafz-Marthalen Flexure (RMF). c, d Comparison of Neuhausen Fault (NHF). Scaling in our models: 10 mm in the model = 100 m in nature

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