Southeastward increase of the late Quaternary slip-rate of the Xianshuihe fault, eastern Tibet. Geodynamic and seismic hazard implications
The left-lateral strike-slip Xianshuihe fault system located in the eastern Tibetan Plateau is considered as one of the most tectonically active intra-continental fault system in China, along which more than 20 M>6.5 and more than 10 M>7 earthquakes occurred since 1700. Therefore, studying its...
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Veröffentlicht in: | Earth and planetary science letters 2018-03, Vol.485, p.19-31 |
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