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- W165169923 abstract "Field investigations allow to constrain the co-seismic surface rupture zone of ~400 km with a strike-slip up to 16.3 m associated with the 2001 Mw 7.8 Central Kunlun earthquake that occurred along the western segment of the Kunlun fault, northern Tibet. The co-seismic rupture structures are almost duplicated on the pre-existing fault traces of the Kunlun fault. The deformational characteristics of the co-seismic surface ruptures reveal that the earthquake had a nearly pure strike-slip mechanism. The geologic and topographic evidence clearly shows that spatial distributions of the co-seismic surface ruptures are restricted by the pre-existing geological structures of the Kunlun fault." @default.
- W165169923 created "2016-06-24" @default.
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- W165169923 date "2004-01-01" @default.
- W165169923 modified "2023-09-28" @default.
- W165169923 title "Relationship between the Pre-existing Active Kunlun Fault and Co-seismic Surface Ruptures Produced by the 2001 Mw7.8Central Kunlun Earthquake,China" @default.
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