| Slip-Rate on the Middle Altyn Tagh Fault since the Holocene Period |
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| 作者姓名： | Wang Feng |
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| 作者单位： | Wang Feng 1)，Li Ming 1)，Xu Xiwei 2) and Zheng Rongzhang 2) 1) China Earthquake Administration，Beijing 100036，China 2) Institute of Geology，China Earthquake Administration，Beijing 100029，China |
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| 基金项目： | National Development of Reform Commission of China Investment |
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| 摘 要： | INTRODUCTIONTheAltynTaghfault,whichliesonthenorthboundaryoftheQinghai Xizang(Tibet)plateau ,runsmorethan 1 50 0kmfromLazhulonginnorthTibettotheKuantanMountainsinGansuprovince ,China.ItiscloselyconnectedtotheformationandevolutionoftheQinghai Xizang(Tibet)p…
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| 关 键 词： | Altyn Tagh断层 滑动走向 地形偏移 全球卫星定位观测 |
Slip-Rate on the Middle Altyn Tagh Fault since the Holocene Period |
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| Wang Feng.Slip-Rate on the Middle Altyn Tagh Fault since the Holocene Period[J].Earthquake Research in China,2005,19(1):64-73. |
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| Authors: | Wang Feng |
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| Institution: | Wang Feng 1),Li Ming 1),Xu Xiwei 2) and Zheng Rongzhang 2) 1) China Earthquake Administration,Beijing 100036,China 2) Institute of Geology,China Earthquake Administration,Beijing 100029,China |
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| Abstract: | |
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| Keywords: | Altyn Tagh fault Strike-slip fault Offset landforms Slip-rate |
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