利用GPS数据反演青藏高原东北缘主要活动断裂滑动速率

李煜航; 崔笃信; 郝明

doi:10.3799/dqkx.2015.158

Volume 40 Issue 10

Oct. 2015

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Li Yuhang, Cui Duxin, Hao Ming, 2015. GPS-Constrained Inversion of Slip Rate on Major Active Faults in the Northeastern Margin of Tibet Plateau. Earth Science, 40(10): 1767-1780. doi: 10.3799/dqkx.2015.158

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Li Yuhang, Cui Duxin, Hao Ming, 2015. GPS-Constrained Inversion of Slip Rate on Major Active Faults in the Northeastern Margin of Tibet Plateau. Earth Science, 40(10): 1767-1780. doi: 10.3799/dqkx.2015.158

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GPS-Constrained Inversion of Slip Rate on Major Active Faults in the Northeastern Margin of Tibet Plateau

doi: 10.3799/dqkx.2015.158

Li Yuhang^{1, 2
,},
Cui Duxin²,
Hao Ming²

1.
Institute of Geology, CEA, Beijing 100029, China
2.
Second Crust Monitoring and Application Center, CEA, Xi'an 710054, China

Received Date: 2014-11-18
Publish Date: 2015-10-15

Abstract

Abstract

GPS mwasurements can provide a high accuracy of spatio-temporal images, but there aren't enough study about it. We use the spherical linear block theory constrained by geodetic observations from Global Positioning System (GPS) stations to estimate fault slip rates on the Northeastern margin of Tibet plateau and spatially variable coupling on Haiyuan fault in abroad sense. The 3D geometric block model is based on the previous researches of active block. The result provides a new constraint and reference for the geodynamics of present crustal deformation and the middle-long term strong earthquake hazard study in this area.
- the Northeastern margin of Tibet plateau,
- spherical linear block theory,
- GPS,
- fault slip rate

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References(72)

References

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GPS-Constrained Inversion of Slip Rate on Major Active Faults in the Northeastern Margin of Tibet Plateau

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