The geological structure and sliding mode of the slopes in the Yigong landslide source area, Tibet

The geological structure and sliding mode of the slopes in the Yigong landslide source area, Tibet

The unstable slopes of BH01, BH02, and BH03 in the Yigong landslide source area in Tibet threaten the safety of major engineering facilities downstream. In order to prevent and control the disaster risk caused by the high-elevation sliding of blocks, it is urgent to analyze the geological structure...

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Bibliographic Details
Main Authors: XIN Peng, WANG Tao, LIU Jiamei, LIU Feng, DU Jianjun, ZHAO Jianlei
Format: Article
Language:zho
Published: Institute of Geomechanics, Chinese Academy of Geological Sciences 2022-12-01
Series:Dizhi lixue xuebao
Subjects:
geological disaster
yigong landslide
source area
imbricated nappe structure
fault
sliding mode
Online Access:https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2022072

Internet

https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2022072

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