| Coseismic landslide sediment increased by the “9.5” Luding earthquake,Sichuan, China |
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| 作者姓名： | XIONG Jiang CHEN Hua-yong ZENG Lu SU Feng-huan GONG Ling-feng TANG Chen-xiao |
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| 作者单位： | 1. Key Laboratory of Mountain Hazards and Earth Surface Processes, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences;2. Chengdu Geological Survey Center,China Geological Survey |
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| 基金项目： | financially supported by the National Natural Science Foundation of China (Grant No. U21A2008)；;Science and Technology Project of Tibet Autonomous Region (Grant No. XZ202101ZD0001G)；;CAS Light of West China Program； |
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| 摘 要： | The "9.5" Luding earthquake(Ms 6.8),which occurred on September 5,2022,has triggered thousands of landslides,and caused coseismic landslide sediment in the mountain basin to increase significantly.After the Luding earthquake,landslide sediment may continue to divert to channels,and increase the activity of debris flows.Importantly,the formation of debris flows can pose a major threat to infrastructure,lives and property.To better understand the landslide sediment that increased by the "9.5" Ludi...
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