Fig. 14From: Evidence for synsedimentary differential tectonic movements in a low-subsidence setting: Early Jurassic in northwestern SwitzerlandPalinspastically restored isopach map of the Gross Wolf Member (Staffelegg Formation) and basal part of the Opalinus-Ton, the Jurensismergel Formation and basal part of the Opalinuston Formation as well as Toarcien marneux and basal part of the marnes à opalinum (Late Toarcian). Permo-Carboniferous troughs and faults simplified after Wetzel (2008)Back to article page