Fig. 12From: Influence of rheologically weak layers on fault architecture: insights from analogue models in the context of the Northern Alpine Foreland BasinSchematic overview depicting the influence of viscous layer properties on model development (in pure normal dip-slip models). a–f Final state of model deformation. g–n Evolution of g–j) sand-only Model A1, and k–n of Model A4 with a standard thickness viscous layerBack to article page