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Erschienen in: Bulletin of Engineering Geology and the Environment 7/2019

18.12.2018 | Original Paper

Process analysis of the Moxi earthquake-induced Lantianwan landslide in the Dadu River, China

verfasst von: Yunsheng Wang, L. Z. Wu, Jin Gu

Erschienen in: Bulletin of Engineering Geology and the Environment | Ausgabe 7/2019

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Abstract

Many large-scale landslides have occurred along the Dadu River, in particular in the middle section of the river, located on the eastern edge of the Qinghai–Tibet Plateau. The large-scale Lantianwan landslide was triggered by the 1786 Moxi earthquake (Ms = 7.75) at Luding, Sichuan province, China. Field investigations and 3D discrete element methods were used to examine the landslide formation mechanism and simulate landslide movement. The evolution of the landslide can be divided into four stages: initiation, high-speed motion, debris flow, and accumulation and river blocking. The results indicate that tension cracking and horizontal sliding were the geological origins of the Lantianwan landslide. The Moxi earthquake combined with the magnifying effect of the topography and the back slope formed deep-dip tensile structural planes in the Lantianwan slope, which triggered the landslide.

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Metadaten
Titel
Process analysis of the Moxi earthquake-induced Lantianwan landslide in the Dadu River, China
verfasst von
Yunsheng Wang
L. Z. Wu
Jin Gu
Publikationsdatum
18.12.2018
Verlag
Springer Berlin Heidelberg
Erschienen in
Bulletin of Engineering Geology and the Environment / Ausgabe 7/2019
Print ISSN: 1435-9529
Elektronische ISSN: 1435-9537
DOI
https://doi.org/10.1007/s10064-018-01438-2

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