Fig. 1From: Dynamic deformation and fault locking of the Xianshuihe Fault Zone, Southeastern Tibetan Plateau: implications for seismic hazardssource: Xu et al. (2013)). The red beach balls represent the typical earthquakes occurred in the study area since 2000Tectonic setting and historic seismicity in the eastern Tibetan Plateau. S1–S5 represent the Luhuo, Daofu, Qianning, Kangding, and Moxi sections, respectively. The gray circles represent M ≥ 6.5 earthquakes since 1970, and the black beach balls represent the focal mechanisms of the M ≥ 6.7 strong earthquakes from 1900 to 2000 (data Back to article page