Fig. 9From: Evidence for synsedimentary differential tectonic movements in a low-subsidence setting: Early Jurassic in northwestern SwitzerlandPalinspastically restored isopach map of the Beggingen and Weissenstein members (Staffelegg Formation), Arietenkalk Formation, Calcaire à Gryphées; Early Sinemurian–early Late Sinemurian. Permo-Carboniferous troughs and faults simplified after Wetzel (2008)Back to article page