川西理塘高原冰蚀湖记录的晚更新世古地震事件

朱宁; 徐亚东; 季军良; 曹凯; 李星波; 孙玲; 邹司雅; 彭绍勇; 易念; 张笛

doi:10.3799/dqkx.2021.125

Volume 48 Issue 9

Sep. 2023

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Article Navigation > Earth Science > 2023 > 48(9): 3562-3576

Zhu Ning, Xu Yadong, Ji Junliang, Cao Kai, Li Xingbo, Sun Ling, Zou Siya, Peng Shaoyong, Yi Nian, Zhang Di, 2023. Late Pleistocene Paleoseismic Events Recorded by Glacial Erosive Lake in the Litang Plateau, Western Sichuan. Earth Science, 48(9): 3562-3576. doi: 10.3799/dqkx.2021.125

Citation:

Zhu Ning, Xu Yadong, Ji Junliang, Cao Kai, Li Xingbo, Sun Ling, Zou Siya, Peng Shaoyong, Yi Nian, Zhang Di, 2023. Late Pleistocene Paleoseismic Events Recorded by Glacial Erosive Lake in the Litang Plateau, Western Sichuan. Earth Science, 48(9): 3562-3576. doi: 10.3799/dqkx.2021.125

Citation:

Zhu Ning, Xu Yadong, Ji Junliang, Cao Kai, Li Xingbo, Sun Ling, Zou Siya, Peng Shaoyong, Yi Nian, Zhang Di, 2023. Late Pleistocene Paleoseismic Events Recorded by Glacial Erosive Lake in the Litang Plateau, Western Sichuan. Earth Science, 48(9): 3562-3576. doi: 10.3799/dqkx.2021.125

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Late Pleistocene Paleoseismic Events Recorded by Glacial Erosive Lake in the Litang Plateau, Western Sichuan

doi: 10.3799/dqkx.2021.125

Zhu Ning^{1, 2
,
,},
Xu Yadong^{2, 3, 4
,
,
,},
Ji Junliang^{2, 4, 5},
Cao Kai²,
Li Xingbo^{2, 5},
Sun Ling^{2, 5},
Zou Siya^{2, 5},
Peng Shaoyong²,
Yi Nian²,
Zhang Di²

1.
China Geological Survey Cores and Samples Centre of Natural Resources, Langfang 065201, China
2.
Hubei Key Laboratory of Critical Zone Evolution, School of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Geological Science and Technology Innovation Center of Central South China, Wuhan 430205, China
4.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430078, China
5.
School of Geography and Information Engineering, China University of Geosciences, Wuhan 430074, China

Received Date: 2021-08-16
Available Online: 2023-10-07
Publish Date: 2023-09-25

Abstract

Abstract

Glacial lacustrine deposit has high-resolution sedimentary records, which has great geological significance. The Quaternary glacial and interglacial events can be recorded by the lacustrine deposit. The Litang Plateau, located in the southeastern margin of the Qinghai-Tibetan Plateau, is the transition zone with the most significant terrain changes in China, and it has well developed glacial landform. A continuous 16 m-thick lacustrine section is measured in the Maoya Basin, western side of the Litang Plateau, which is formed in a glacial-dammed lake. It is composed of laminated mud and silty sand layers, and the soft-sediment deformation structures at the depth ranging from 12.68 to13.26 m were triggered by earthquake events. The main structures of the pliable sediment deformation include liquefied curling deformed layer, ball-pillow structure, liquefied diapir and interlayer slipping fold deformation, morphologically. Based on the AMS ¹⁴C radionuclide dating, the age interval is obtained at 33 850-33 110 cal. BP and 37 254-36 042 cal. BP. It indicates that at least two paleoseismic events occurred in this area during ± 37-33 ka. The earlier event occurred before 37-36 ka with magnitude above 7, and the later event occurred after 33 ka, with magnitude of around 6-7.
- Litang Plateau,
- glacial-dammed lake,
- Late Pleistocene,
- soft-sediment deformation,
- paleoseismic events,
- stratigraphy,
- particle size analysis

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References(77)

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