Fig. 1.From: Microstructural characterization of natural fractures and faults in the Opalinus Clay: insights from a deep drilling campaign across central northern SwitzerlandGeological setting a Simplified tectonic map of central northern Switzerland with selected Nagra boreholes (Nagra, 2014). b Generic stratigraphic column with the approximately 110 m thick Opalinus Clay. c Regional cross sections. Upper section across the Jura fold-and-thrust belt and the lower section orthogonal to the trend of the Hegau-Lake Constance Graben (Jordan et al., 2015)Back to article page