Fig. 13
From: Structure, geometry and kinematics of the northern Adula nappe (Central Alps)
Stereographic projections of structural data from the northern Adula nappe (for locations of subareas, see Fig. 14b). The lineations in the northwest Adula are principally attributed to LL; the lineations are not separated between different deformation phases because LL is nearly indistinguishable from LZ. The best-fit girdle and the beta axis indicating the fold axis of the Carassino-antiform (plunging 14° towards 066°) are shown. Lambert equal-area projection, lower hemisphere