Fig. 10From: Evidence for synsedimentary differential tectonic movements in a low-subsidence setting: Early Jurassic in northwestern SwitzerlandPalinspastically restored isopach map of the Frick, Grünschholz, Fasiswald members and basal part of the Mt. Terri Member as well as the Obtusus Formation and Lotharingien (early Late Sinemurian–Early Pliensbachian). Permo-Carboniferous troughs and faults simplified after Wetzel (2008)Back to article page