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- W2900930360 abstract "The 14 April 2010 MW 6.9 Yushu earthquake ruptured the northwestern segment of the Ganzi-Yushu Fault in Qinghai,China.Accurate estimation of the secular slip rate across the fault would help understand tectonic structure of the fault and its seismogenic process.GPS data obtained from 1999 to 2007around the Ganzi-Yushu Fault spanning 89°～103°E,28°～39°N make such estimation possible.After removing GPS stations whose displacements were affected by fault locking effects and/or deformation of other faults,we decompose the remaining GPS station velocities into strike-parallel and strike-normal components and examine the data along profiles across corresponding fault segments.The slip rates of the Fenghuoshan,Ganzi-Yushu,and northwestern segment of the Xianshuihe Faults are estimated as 6.1±1.9,6.6±1.5,and 10.2±0.7mm/a,respectively.These results agree with geological estimates of the fault slip rates,which show progressive increase from northwest to southeast across segments of the Ganzi-Yushu-Xianshuihe Fault zone,implying variation in transferring and absorbing patterns of deformation in different regions in and around the Tibetan plateau.Estimation of present-day slip rates along segments of the Ganzi-Yushu Fault would provide valuable data for future research on seismo-tectonics of the fault and tectonic evolution of the Tibetan plateau." @default.
- W2900930360 created "2018-11-29" @default.
- W2900930360 creator A5089657946 @default.
- W2900930360 date "2011-01-01" @default.
- W2900930360 modified "2023-09-23" @default.
- W2900930360 title "INTER-SEISMIC DEFORMATION FIELD OF THE GANZI-YUSHU FAULT BEFORE THE 2010 YUSHU EARTHQAUKE" @default.
- W2900930360 hasPublicationYear "2011" @default.
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