Fig. 8From: Dynamic deformation and fault locking of the Xianshuihe Fault Zone, Southeastern Tibetan Plateau: implications for seismic hazardsLocking degree in the Xianshuihe Fault Zone. a and b The locking degrees of the Xianshuihe Fault Zone in 1999–2007 and 2016–2020. S1–S5 represent the Luhuo, Daofu, Qianning, Kangding, and Moxi sections, respectivelyBack to article page