Kinematic and Mechanical Heterogeneity Along the Xianshuihe Fault Zone from Nine Years of Continuous Seismicity and a Crustal Velocity Model
The Xianshuihe fault zone (XSHF), a major strike-slip system on the southeastern Tibetan Plateau, is one of the most seismically active structures in China. However, the relationship between its kinematics and long-term seismic behavior remains poorly understood. Here, we utilize continuous seismic data from 2014 to...