Field structures and microstructures in the granitoids. (a): S_m magmatic fabric reoriented by C_n+1 synmagmatic sinistral shear zone, (b): magmatic texture with euhedral feldspar crystals, (c): myrmekitic buds along plagioclase rim, (d): chessboard pattern of quartz crystal, (e): plagioclase affected by kink band and damouritization, (f): mylonite fabric defined by quartz ribbons, (g): anticlockwise bookshelf structure, (h): asymmetric porphyroclasts of feldspars describing the sinistral motion.