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The Holocene Activity Evidence of the Yema River-Daxue Mountain Fault in Western Qilian Mountain

LUO Hao HE Wengui YUAN Daoyang SHAO Yanxiu

地质学报（英文版）2013，Vol.87Issue(6)：1569-1584,16.

The Holocene Activity Evidence of the Yema River-Daxue Mountain Fault in Western Qilian Mountain

LUO Hao ¹HE Wengui ²YUAN Daoyang ³SHAO Yanxiu²

作者信息

1. Key Laboratory of Engineering Geomechanics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2. Earthquake Research Institute of Lanzhou, China Earthquake Administration, Lanzhou 730000,Gansu, China
3. Lanzhou National Geophysical Observatory, Lanzhou 73000, Gansu, China
折叠

摘要

关键词

paleoearthquake/earthquake recurrence interval/reference magnitude/Yema River-Daxue Mountain fault/Altyn Tagh fault

Key words

paleoearthquake/earthquake recurrence interval/reference magnitude/Yema River-Daxue Mountain fault/Altyn Tagh fault

引用本文复制引用

LUO Hao,HE Wengui,YUAN Daoyang,SHAO Yanxiu..The Holocene Activity Evidence of the Yema River-Daxue Mountain Fault in Western Qilian Mountain[J].地质学报（英文版）,2013,87(6):1569-1584,16.

基金项目

This work is granted by the National Natural Science Foundation of China (Grant No.40872132,41030317) and Chinese Academy of Sciences Key Project XDB03020201. （Grant No.40872132,41030317）

地质学报（英文版）

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ISSN：1000-9515

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