EMERGENCY RAPID ASSESSMENT OF LANDSLIDES INDUCED BY THE JIUZHAIGOU <i>M</i><sub>S</sub> 7.0 EARTHQUAKE, SICHUAN, CHINA

LIU Jiamei; WANG Tao; SHI Jusong; LI Zetong

Volume 23 Issue 5

Oct. 2017

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Article Navigation > Journal of Geomechanics > 2017 > 23(5): 639-645

HUANG Xiao-long, WU Zhong-hai, WU Kun-gang, et al., 2016. THE MAIN ACTIVE FAULTS AND TECTONIC SYSTEM IN YONGSHENG AREA, NORTHWESTERN YUNNAN. Journal of Geomechanics, 22 (3): 531-547.

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LIU Jiamei, WANG Tao, SHI Jusong, et al., 2017. EMERGENCY RAPID ASSESSMENT OF LANDSLIDES INDUCED BY THE JIUZHAIGOU M_S 7.0 EARTHQUAKE, SICHUAN, CHINA. Journal of Geomechanics, 23 (5): 639-645.

HUANG Xiao-long, WU Zhong-hai, WU Kun-gang, et al., 2016. THE MAIN ACTIVE FAULTS AND TECTONIC SYSTEM IN YONGSHENG AREA, NORTHWESTERN YUNNAN. Journal of Geomechanics, 22 (3): 531-547.

Citation:

LIU Jiamei, WANG Tao, SHI Jusong, et al., 2017. EMERGENCY RAPID ASSESSMENT OF LANDSLIDES INDUCED BY THE JIUZHAIGOU M_S 7.0 EARTHQUAKE, SICHUAN, CHINA. Journal of Geomechanics, 23 (5): 639-645.

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EMERGENCY RAPID ASSESSMENT OF LANDSLIDES INDUCED BY THE JIUZHAIGOU M_S 7.0 EARTHQUAKE, SICHUAN, CHINA

LIU Jiamei^{1, 2
,},
WANG Tao^{1, 2
,
,},
SHI Jusong³,
LI Zetong^{1, 2}

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing, 100081, China
2.
Key Laboratory of Neotectonic Movement and Geohazard, Ministry of Land and Resourses, Beijing, 100081, China
3.
China Geological Survey, Beijing, 100037, China

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Abstract

Abstract

Based on the Newmark cumulative displacement model, emergency rapid assessment of earthquake landslides induced by the Sichuan Jiuzhaigou M_s 7.0 earthquake was carried out based on regional topographic and geologic data, combined with near-real-time estimates of ground shaking. The analysis results of seismic landslide displacements show that the medium-high risk zones of coseismic landslide activities are mainly concentrated in the area about 4 km width along the seismogenic fault, with a roughly NW-SE rift direction, especially in the Fengxuetang, Rize, and Ganhaizi town of the meizoseismal area. Comparison between the satellite images acquired before and after this earthquake shows that the most common types of landslides induced by the Jiuzhaigou earthquake are shallow debris flows and small scale of rock falls, and the shallow debris flows are mostly formed by the further expansion of activities of the existing landslides. It shows that the obtained displacements can well reflect the macro distribution of coseismic landslide, but they can't be exerted effectively at local site scale, which can be enhanced through the improvement of large scale of geologic maps and high quality topography data. Results can provide valuable timely reference information on the possible societal effects of earthquake-induced landslides.
- The Jiuzhaigou earthquake,
- seismic landslide hazard,
- emergency rapid assessment,
- Newmark cumulative displacement model

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References

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EMERGENCY RAPID ASSESSMENT OF LANDSLIDES INDUCED BY THE JIUZHAIGOU M_S 7.0 EARTHQUAKE, SICHUAN, CHINA

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EMERGENCY RAPID ASSESSMENT OF LANDSLIDES INDUCED BY THE JIUZHAIGOU MS 7.0 EARTHQUAKE, SICHUAN, CHINA

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EMERGENCY RAPID ASSESSMENT OF LANDSLIDES INDUCED BY THE JIUZHAIGOU M_S 7.0 EARTHQUAKE, SICHUAN, CHINA