Geometry, Slip Rate, and the Latest Earthquake of the Jinta Nanshan Fault: Interactions of the Altyn Tagh Fault and the Qilian Shan at the Northern Margin of the Tibetan Plateau-Reference-Cited by-同舟云学术

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Geometry, Slip Rate, and the Latest Earthquake of the Jinta Nanshan Fault: Interactions of the Altyn Tagh Fault and the Qilian Shan at the Northern Margin of the Tibetan Plateau

Published:2023 Issue: Volume: Page:
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Author:

Zhang Bo,Allen Mark B.,Yao Yunsheng,Zhu Junwen,Wu Ming,Wang Weitong,Wen Yameng,He Wengui,Lei Zhongsheng,Pang Wei

Publisher

Elsevier BV

Reference53 articles.

1. Evidence from the Qilian Shan, northeastern Tibetan Plateau;Tectonics

2. Geodetic evidence for a low slip rate in the Altyn Tagh fault system;R Bendick;Nature,2000

3. Constraining the Distribution of Vertical Slip on the South Heli Shan Fault (Northeastern Tibet) From High-Resolution Topographic Data;H Bi;Journal of Geophysical Research: Solid Earth,2018

4. Sinistral strike-slip faults along the southern Alashan margin and eastwards extending of the Altun fault;W Chen;Seismoglogy and Geology,2006

5. Models of crustal flow in the India-Asia collision zone;A Copley;Geophysical Journal International,2007

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