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: | , , , , , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
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De Gruyter
2024-11-01
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| Edice: | Open Geosciences |
| Témata: | |
| On-line přístup: | https://doi.org/10.1515/geo-2022-0715 |
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