Fig. 8From: Evidence for synsedimentary differential tectonic movements in a low-subsidence setting: Early Jurassic in northwestern SwitzerlandPalinspastically restored isopach map of the Base Beggingen Member (Staffelegg Formation), Angulatenton Formation, Lumachelle à Angulata; Late Hettangian. Permo-Carboniferous troughs and faults simplified after Wetzel (2008)Back to article page