Fig. 13

Palaeo-escarpments sealed by Tertiary formations—examples from the Sanetsch area (for location, see Fig. 1): a anticline–syncline structure affected by normal faults (violet dashed lines). The top of the Klimsenhorn Formation seals the faults (dotted orange line). b Normal palaeo-faults that terminate beneath the erosive surface onlapped by the Klimsenhorn Formation deposits, demonstrating that faulting is older than Eocene. c Angular unconformity between Lower Cretaceous and Tertiary beds (588805/134483)