Fig. 9From: Inherited structural controls on fault geometry, architecture and hydrothermal activity: an example from Grimsel Pass, SwitzerlandCross section across the Sidelhorn Linkage Zone. Marked from Z to Z’ on Fig. 3 with the same symbology. The major SZs are projected (after Baumberger 2015) to 2 km depth below surface, based on the surface trace over the steep topography, field-collected dip data, and the Transitgas tunnel intersectionBack to article page