Physics
Scientist
Institute of Crustal Dynamic, State Seismological Bureau, Beijing 100085, People's Republic of China
Uniform postglacial slip-rate along the central 600km of the Kunlun Fault (Tibet), from 26 Al, 10 Be, and 14 C dating of riser offsets, and climatic origin of the regional morphology
Uniform Slip-Rate along the Kunlun Fault: Implications for seismic behaviour and large-scale tectonics
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