Fig. 2From: Re-evaluation of the activity of the Thoen Fault in the Lampang Basin, northern Thailand, based on geomorphology and geochronologyMajor tectonic elements in SE Asia and adjacent areas. Arrows show relative directions of plate movement during the late Cenozoic. TPFZ—Three Pagodas Fault Zone; MPFZ—Mae Ping Fault Zone; UFZ—Uttaradit Fault Zone. (Modified from Polachan et al., 1991).Back to article page