“…The focal mechanisms of these earthquakes, GPS data (Wang et al, ), and in situ stress measurements all imply that nearly east–west compression has resulted in right‐lateral strike‐slip with a reverse slip component on the faults (Hsiao et al, ; Li et al, ; Liu et al, , ; Yin et al, ; Zhu et al, ). Studies of paleo‐earthquakes and shallow seismic profiles have also revealed significant activity of the TLFZ in the late Quaternary (Huang, Liu, & Kusky, ; Liu, Zhu, Zhai, Gu, & Liu, ; Min, Jiao, Zhou, Shen, & Chen, ; Min, Liu, Jiao, Shen, & Pan, ; Yin et al, ; Zhu et al, ). This fault has become a focus of research because of its seismicity and potential risk in the late Quaternary (Min et al, , ; Yu, ; Zhang et al, ; Zhu et al, ).…”