Fig. 1From: Evidence for synsedimentary differential tectonic movements in a low-subsidence setting: Early Jurassic in northwestern SwitzerlandPalinspastically restored isopach map of the Early Jurassic in NW Switzerland and adjacent parts of France and Germany (modified after Reisdorf et al. 2011). Contrary to Reisdorf et al. (2011: Fig. 6), the thickness of the basal part of the Opalinus-Ton/Opalinuston Formation (Torulosum subzone, Late Toarcian) is now includedBack to article page