The thrust at the base of the horse of Urgonian - carrying it onto a
footwall of Upper Cretaceous marls and limestones. Notice the intensely brecciated
(rubbly) rock below the overhanging fault surface (being studied by the geologist in the
photograph). This fault breccia is characteristic of the main thrusts in the Chartreuse.
The main fault plane has been measured in two places:
1. fault surface 032-44SE,
striations plunge 42 towards 099
2. fault surface 034 -26SE, striations
plunge 22 towards 110. |