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Evidence of late quaternary activity of the Weining-Shuicheng Fault in Guizhou, China

The Weining-Shuicheng Fault (WSF) is a northwest-southeast trending fault in the southwest of the South China Block (SCB), which is an important component of the Yadu-Ziyun Fault Zone. The study of its activity is of great significance for analyzing the boundary role of the Daliangshan secondary blo...

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Hlavní autoři: Ji Xingxing, Wang Jiahai, Liu Hao, Hao Jing, Ruan Jie, Li Cheng, Zhang Wei, Asghar Aamir
Médium: Artigo
Jazyk:Inglês
Vydáno: De Gruyter 2024-11-01
Edice:Open Geosciences
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On-line přístup:https://doi.org/10.1515/geo-2022-0715
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