Holocene activity and seismic surface rupture zone of the Abuduo fault eastern Tibetan Plateau

Holocene activity and seismic surface rupture zone of the Abuduo fault eastern Tibetan Plateau

The Garzê–Yushu fault is a large active NW-trending strike-slip fault on the Tibetan Plateau, along which strong earthquakes have frequently occurred historically. Together with the Xianshuihe fault, the Garzê–Yushu fault constitutes the northern boundary of the Sichuan–Yunnan block, and it is also...

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Bibliographic Details
Main Authors: Cheng Liao, Mingjian Liang, Han Chen, Zebin Mao, Weiwei Wu, Yue Gong, Hong Zuo, Shuhuai Liu, Tian Li, Zhongyang Li
Format: Article
Language:English
Published: Frontiers Media S.A. 2024-01-01
Series:Frontiers in Earth Science
Subjects:
Abuduo fault
Garzê–Yushu fault
Holocene activity
surface rupture
Tibetan plateau
Online Access:https://www.frontiersin.org/articles/10.3389/feart.2024.1351970/full

Internet

https://www.frontiersin.org/articles/10.3389/feart.2024.1351970/full

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