Fig. 11
Outcrop photograph and structural data of phyllonite in the Yuli Belt along south bank of the western Chingsuei River (see Fig. 5 for location). A Photograph of well-developed phyllonite, parallel to pencil and later shear zone interpreted to be S3. View southwest. B Orientation data for S2, and S3, fabrics in A. Movement direction (black arrows) is inferred from asymmetric folds associated with S3 and shows west-side down