Fig. 9From: Dynamic deformation and fault locking of the Xianshuihe Fault Zone, Southeastern Tibetan Plateau: implications for seismic hazardsFault-parallel slip-rate deficit in the Xianshuihe Fault Zone. a and b The fault-parallel slip-rate deficits in 1999–2007 and 2016–2020. S1–S5 represent the Luhuo, Daofu, Qianning, Kangding, and Moxi sections, respectivelyBack to article page