Nature and timing of a prehistoric giant landslide on the eastern margin of the Tibetan Plateau
文献类型:期刊论文
作者 | Zhao, Xun3; Wang, Yun-sheng3; Wang, Shi-yuan1; Zhao, Bo2![]() |
刊名 | JOURNAL OF MOUNTAIN SCIENCE
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出版日期 | 2020-06-01 |
卷号 | 17期号:6页码:1438-1451 |
关键词 | Prehistoric landslide Active fault zone Palaeo-seismic episode Dating |
ISSN号 | 1672-6316 |
DOI | 10.1007/s11629-019-5831-y |
产权排序 | 3 |
通讯作者 | Zhao, Xun(zhaoxun1989@163.com) ; Wang, Yun-sheng(wangys60@163.com) ; Wang, Shi-yuan(544756125@qq.com) |
文献子类 | Article |
英文摘要 | Studying the characteristics of a prehistoric giant landslide and ascertaining its relationship with palaeo-seismic events could provide useful information on the role of regional tectonic activities in hillslope evolution. Here, a giant palaeoseismic landslide (GPSL), namely, the Luanshibao (LSB) landslide, located on the eastern margin of the Qinghai-Tibet Plateau, was investigated to ascertain its characteristics and occurrence age. The relationship between occurrence age and palaeoseismic episodes was also discussed by using 14C dating on the adjacent active faults, including the regional Yidun-Litang-Dewu (YD-LT-DW) fault zone, which crossed the LSB landslide. The dating of multiple samples acquired from palaeo-seismic trenches revealed that at least 5 palaeo-seismic episodes had occurred in the vicinity of the LSB landslide over the last 5000 years. The occurrence age of the LSB landslide (3635 +/- 387 a BP) coincides with palaeo-seismic episode I, and the LSB landslide is convincingly inferred to have been triggered during episode I, which reached a seismic intensity (Chinese scale) of at least degree VII near the LSB landslide during failure. The timing of a second reactivation phase coincides with palaeo-seismic episode IV, which occurred at 2100-2200 a BP. The study could provide reference for studying the regional palaeoseismic activities and palaeo landslide evolution near the Litang area. |
电子版国际标准刊号 | 1993-0321 |
WOS关键词 | SICHUAN PROVINCE ; DAMMED LAKE ; EARTHQUAKE ; NORTHERN ; RIVER ; MAGNITUDES ; EROSION |
WOS研究方向 | Environmental Sciences & Ecology |
语种 | 英语 |
WOS记录号 | WOS:000538038700012 |
出版者 | SCIENCE PRESS |
源URL | [http://ir.imde.ac.cn/handle/131551/34882] ![]() |
专题 | 成都山地灾害与环境研究所_山地灾害与地表过程重点实验室 |
通讯作者 | Zhao, Xun |
作者单位 | 1.Sichuan Earthquake Agcy, Chengdu 610041, Sichuan, Peoples R China; 2.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Earth Surface Proc, Chengdu 610041, Peoples R China 3.Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Pro, Chengdu 610059, Peoples R China; |
推荐引用方式 GB/T 7714 | Zhao, Xun,Wang, Yun-sheng,Wang, Shi-yuan,et al. Nature and timing of a prehistoric giant landslide on the eastern margin of the Tibetan Plateau[J]. JOURNAL OF MOUNTAIN SCIENCE,2020,17(6):1438-1451. |
APA | Zhao, Xun.,Wang, Yun-sheng.,Wang, Shi-yuan.,Zhao, Bo.,Zeng, Lu.,...&Feng, Qian-qian.(2020).Nature and timing of a prehistoric giant landslide on the eastern margin of the Tibetan Plateau.JOURNAL OF MOUNTAIN SCIENCE,17(6),1438-1451. |
MLA | Zhao, Xun,et al."Nature and timing of a prehistoric giant landslide on the eastern margin of the Tibetan Plateau".JOURNAL OF MOUNTAIN SCIENCE 17.6(2020):1438-1451. |
入库方式: OAI收割
来源:成都山地灾害与环境研究所
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