Paleoseismic events and ages revealed by the Lianhuashan trench in the western section of the Tuyouqi of the Daqingshan piedmont fault

Daqingshan piedmont fault is located in the northern margin of Hetao basin and has been active strongly since the Late Quaternary. Previous researchers had conducted extensive research on the characteristics of paleoseismic in this area, but limited by the dating techniques and the fact that there w...

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Hlavní autoři:	Yunsheng Yao, Aiguo Wang, Yanxiu Shao, Xingwang Liu, Bo Zhang, Yuanyuan Jia
Médium:	Artigo
Jazyk:	Chinês
Vydáno:	Editorial Office of Progress in Earthquake Sciences 2024-01-01
Edice:	地震科学进展
Témata:	daqingshan piedmont fault western section of tuyouqi lianhuashan paleoseismic trench recurrence interval normal fault
On-line přístup:	https://www.gjdzdt.cn/en/article/doi/10.19987/j.dzkxjz.2023-132
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