Distribution patterns of landslides triggered by the 2022 MS 6.8 Luding earthquake, Sichuan, China
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作者:
ZHANG Jian-qiang
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机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
ZHANG Jian-qiang
[1
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YANG Zong-ji
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
YANG Zong-ji
[1
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MENG Qing-kai
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
MENG Qing-kai
[1
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WANG Jiao
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
WANG Jiao
[1
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HU Kai-heng
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
HU Kai-heng
[1
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GE Yong-gang
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
GE Yong-gang
[1
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SU Feng-huan
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
SU Feng-huan
[1
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ZHAO Bo
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
ZHAO Bo
[1
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ZHANG Bo
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
ZHANG Bo
[1
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JIANG Ning
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h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
JIANG Ning
[1
,2
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HUANG Yu
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
East China University of TechnologyInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
HUANG Yu
[1
,3
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MING Zai-yang
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
East China University of TechnologyInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
MING Zai-yang
[1
,3
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ZHANG Yi-fan
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
ZHANG Yi-fan
[1
,2
]
LIU Zhen-xing
论文数: 0引用数: 0
h-index: 0
机构:
University of Chinese Academy of Sciences
Institute of Geographic Sciences and Natural Resources ResearchInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
LIU Zhen-xing
[2
,4
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WU Chun-hao
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
WU Chun-hao
[1
,2
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ZHOU Wen-tao
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
ZHOU Wen-tao
[1
,2
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LIANG Xin-yue
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
LIANG Xin-yue
[1
,2
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SUN Yu-qing
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
SUN Yu-qing
[1
,2
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YANG Lian-bing
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
YANG Lian-bing
[1
,2
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YAO Hong-kun
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
YAO Hong-kun
[1
,2
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FENG Pei-hua
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
Chongqing Jiaotong UniversityInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
FENG Pei-hua
[1
,5
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LIU Jia-li
论文数: 0引用数: 0
h-index: 0
机构:
Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
University of Chinese Academy of SciencesInstitute of Mountain Hazards and Environment, Chinese Academy of Sciences
LIU Jia-li
[1
,2
]
机构:
[1] Institute of Mountain Hazards and Environment, Chinese Academy of Sciences
[2] University of Chinese Academy of Sciences
[3] East China University of Technology
[4] Institute of Geographic Sciences and Natural Resources Research
At 12:52 pm on September 5, 2022, an MS 6.8 earthquake occurred in Luding County, Sichuan Province, China. Based on high-resolution aerial photographs and satellite imageries obtained after the earthquake, as well as field investigation, a total of 8685 earthquake-triggered landslides(EQTLs) were interpreted. The landslides covered an area of 30.7km2, with a source area of 9.4 km2. These EQTLs were mainly distributed in areas with a seismic intensity of VIII and IX. Most of the landslides were small and medium in size, and their types included landslide,rockfall, and rock slump. Characteristic landslide distributions were found, EQTLs were distributed along the Xianshuihe fault, landslide area decreased gradually with an increased distance to the fault;EQTLs were distributed along the Daduhe River and roads; besides, landslide distribution was associated with ground deformation caused by the earthquake.EQTLs’ characteristics indicated that, a large number of EQTLs were located near the foot of the slope; the full area of EQTLs and their source area followed a power function. This study concluded that Luding EQTLs were greater in number and area but relatively smaller in terms of affected area. Investigations on geo-hazards post-earthquake and risk assessment were proposed in the earthquake-stricken area to support the rehabilitation and reconstruction.