Fig. 6
a Scaly fabric in marls and marl-rich limestones developed during synsedimentary extension. The marl flakes represent the foliation planes (S) and are dissected by shear planes (C). Slickensides on C-plane are indicated by a white arrow. b Shear indicators derived from scaly fabrics and asymmetric drag folds from locations Krinnenspitze (left) and Rauth (right) indicating top SW to top SE normal faulting