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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

LUO Hao HE Wengui YUAN Daoyang SHAO Yanxiu

地质学报（英文版）2015，Vol.89Issue(2)：561-574,14.
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地质学报（英文版）2015，Vol.89Issue(2)：561-574,14.

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

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

LUO Hao 1HE Wengui 2YUAN Daoyang 3SHAO Yanxiu4

作者信息

  • 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 Institute of Seismology, China Earthquake Administration, Lanzhou 730000, China
  • 4. Lanzhou National Geophysical Observatory, Lanzhou 730000, China
  • 折叠

摘要

关键词

Slip rate/strike-slip fault/Yema River-Daxue Mountain fault/Altyn Tagh fault/Qilian ranges

Key words

Slip rate/strike-slip fault/Yema River-Daxue Mountain fault/Altyn Tagh fault/Qilian ranges

引用本文复制引用

LUO Hao,HE Wengui,YUAN Daoyang,SHAO Yanxiu..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[J].地质学报（英文版）,2015,89(2):561-574,14.

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). （Grant No.201408023）

地质学报（英文版）

OACSCD

1000-9515

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