Fig. 5From: Dynamic deformation and fault locking of the Xianshuihe Fault Zone, Southeastern Tibetan Plateau: implications for seismic hazardsPrincipal and maximum shear strain rate fields around the Xianshuihe Fault Zone. a and b The results during 1999–2007 and 2016–2020. The black arrows represent the principal strain rates; and the background contours represent the maximum shear strain rateBack to article page