Fig. 5From: Brittle faulting in the Rawil depression: field observations from the Rezli fault zones, Helvetic nappes, Western Switzerlanda Simplified sketch of the tectonic situation in our study area, derived from Fig. 3a, with only the RFZ and the Eocene Klimsenhorn Formation indicated. b Three superimposed cross-sections through the study area. Profile 1 is located to the north of RZF1, profile 2 is located between RFZ1 and RFZ2, and profile 3 is located to the south of RZF2. The three profiles allow a first-order approximation of the total displacement across the fault zones with the help of the large-scale syncline exposed in the study area (Fig. 2d) by correlating constructed fold hinges of the Eocene Klimsenhorn Fm on either side of the fault zonesBack to article page