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Slip Rate of Yema River–Daxue Mountain Fault since the Late Pleistocene and Its Implications on the Deformation of the Northeastern Margin of the Tibetan Plateau
作者姓名:LUO Hao  HE Wengui  YUAN Daoyang  SHAO Yanxiu
作者单位:1 Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China.2 Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China.3 Lanzhou National Geophysical Observatory, Lanzhou 730000, China
基金项目:This work is granted by the Special Fund for China Earthquake Research (Grant No. 201408023), National Natural Science Foundation of China (Grant No. 40872132, 41030317) and Chinese Academy of Sciences Key Project (XDB03020201).
摘    要:The slip rate of Yema River–Daxue Mountain fault in the western segment of Qilian Mountains was determined by the dated offset of river risers or gullies. Results indicate that the left-lateral fault slip rate is 2.82 ± 0.20 mm/a at Dazangdele site,2.00 ± 0.24 mm/a at Shibandun site,and 0.50 ± 0.36 and 2.80 ± 0.33 mm/a at two sites in Zhazihu. The ideal average slip rate of the whole fault is 2.81 ± 0.32 mm/a. The lower slip rate confirms part of the displacement of Altyn Tagh fault was transformed into an uplifting of the strap mountains in the western segment of Qilian Mountains,whereas another part transformed into sinistral displacement of Haiyuan fault. This study illustrates that the slip of large strike-slip faults in the northeastern margin of the plateau transforms into crust thickening at the tip of the fault without large-scale propagation to the outer parts of the plateau.

关 键 词:Slip  rate  strike-slip  fault  Yema  River-Daxue  Mountain  fault  Altyn  Tagh  fault  Qilian  ranges
收稿时间:2013/11/9 0:00:00
修稿时间:9/9/2014 12:00:00 AM

Slip Rate of Yema River-Daxue Mountain Fault since the Late Pleistocene and Its Implications on the Deformation of the Northeastern Margin of the Tibetan Plateau
Authors:LUO Hao  HE Wengui  YUAN Daoyang and SHAO Yanxiu
Institution:1. Key Laboratory of Active Tectonics and Volcano, Institute of Geology, China Earthquake Administration, Beijing 100029, China;Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China
2. Lanzhou Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China ;Lanzhou National Geophysical Observatory, Lanzhou 730000, China
Abstract:
Keywords:Slip rate  strike-slip fault  Yema River-Daxue Mountain fault  Altyn Tagh fault  Qilian ranges
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