Geometry and late Pleistocene slip rates of the Liangdang-Jiangluo fault in the western Qinling mountains, NW China
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- 作者：Zheng Wen-juna ; b ; gszhwj@163.com" class="auth_mail" title="E-mail the corresponding author ; gszhwj@ies.ac.cn" class="auth_mail" title="E-mail the corresponding author ; Liu Xing-wangc ; d ; Yu Jing-xingb ; Yuan Dao-yangc ; Zhang Pei-zhena ; b ; Ge Wei-pengb ; c ; Pang Jian-zhangb ; Liu Bai-yunc
- 关键词：Late Pleistocene slip rates ; Liangdang-Jiangluo fault (LJF) ; Decadal GPS measurement ; Fault geometry ; Deformation transformation ; The western Qinling mountains
- 刊名：Tectonophysics
- 出版年：2016
- 出版时间：26 September 2016
- 年：2016
- 卷：687
- 期：Complete
- 页码：1-13
- 全文大小：4904 K
文摘
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Average thrust and strike slip rate of Liangdang-Jiangluo fault is determined.
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The slip rates of faults on the western QL mountains are around 1 mm/a or lower.
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The decadal GPS velocity suggests that WQL is experiencing slow motions.
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The NWW-trending faults of the WQL played a role in deformation transformation.
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The slip rate of EKLF is not transferred to the WQLF or further north.
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