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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| Asıl Yazarlar: | , , , , , |
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| Materyal Türü: | Artigo |
| Dil: | Chinês |
| Baskı/Yayın Bilgisi: |
Editorial Office of Progress in Earthquake Sciences
2024-01-01
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| Seri Bilgileri: | 地震科学进展 |
| Konular: | |
| Online Erişim: | https://www.gjdzdt.cn/en/article/doi/10.19987/j.dzkxjz.2023-132 |
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