中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Relationship between the spatial distribution of landslides and rock mass strength, and implications for the driving mechanism of landslides in tectonically active mountain ranges

文献类型:期刊论文

作者Wang, Xueliang3,4,5; Clague, John J.2; Crosta, Giovanni Battista1; Sun, Juanjuan3,4,5; Stead, Douglas2; Qi, Shengwen3,4,5; Zhang, Luqing3,4,5
刊名ENGINEERING GEOLOGY
出版日期2021-10-01
卷号292页码:8
关键词Landslide Spatial distribution Rock mass strength Mechanism of landslide Tectonically active mountain ranges Southeastern Tibet
ISSN号0013-7952
DOI10.1016/j.enggeo.2021.106281
英文摘要The relationship between landslides and rock mass strength is fundamental for assessing landslide hazards. Some researchers have proposed that there is an inverse relationship between the number of landslides and rock mass strength. However, in some tectonically active mountain ranges, higher rates of landsliding appear to be associated with greater rock mass strength. We investigated the relation between landslides and rock mass strength in the Langxian (LX), Lulang (LL), and Tongmai (TM) regions in southeastern Tibet by identifying and mapping 294 large bedrock landslides using 10-m resolution lidar bare-earth imagery. An inverse relationship between topographic relief and the slope angle of historical landslides demonstrates that rock mass strength is an important factor controlling relief in the study area. Applying Culmann's method, we back-calculated rock mass strengths ranging from 60 to 770 kPa at the landscape scale. Our data show that, at the landscape scale, more landslides have occurred on the hillslopes with greater rock mass strength than on those with lower rock mass strength. We conclude that the stability of slopes in our study areas is controlled by rock mass strength, but the dominant drivers of failure are rock uplift and river incision, rather than a reduction in rock strength as has been proposed in some tectonically passive regions.
WOS关键词RIVER INCISION ; EARTHQUAKE ; RATES ; CLASSIFICATION ; MORPHOLOGY ; HISTORY ; HAZARD ; UPLIFT ; OSO
资助项目National Key R&D Program of China[2019YFC1509703] ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP)[2019QZKK0904] ; Foundation of China Scholarship Council
WOS研究方向Engineering ; Geology
语种英语
WOS记录号WOS:000692696200036
出版者ELSEVIER
资助机构National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; National Key R&D Program of China ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Second Tibetan Plateau Scientific Expedition and Research Program (STEP) ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council ; Foundation of China Scholarship Council
源URL[http://ir.iggcas.ac.cn/handle/132A11/102633]  
专题地质与地球物理研究所_中国科学院页岩气与地质工程重点实验室
通讯作者Wang, Xueliang
作者单位1.Univ Milano Bicocca, Dept Earth & Environm Sci, Piazza Sci 4, I-20126 Milan, Italy
2.Simon Fraser Univ, Dept Earth Sci, Burnaby, BC V5A 1S6, Canada
3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
4.Chinese Acad Sci, Innovat Acad Earth Sci, Beijing 100029, Peoples R China
5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Shale Gas & Geoengn, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714
Wang, Xueliang,Clague, John J.,Crosta, Giovanni Battista,et al. Relationship between the spatial distribution of landslides and rock mass strength, and implications for the driving mechanism of landslides in tectonically active mountain ranges[J]. ENGINEERING GEOLOGY,2021,292:8.
APA Wang, Xueliang.,Clague, John J..,Crosta, Giovanni Battista.,Sun, Juanjuan.,Stead, Douglas.,...&Zhang, Luqing.(2021).Relationship between the spatial distribution of landslides and rock mass strength, and implications for the driving mechanism of landslides in tectonically active mountain ranges.ENGINEERING GEOLOGY,292,8.
MLA Wang, Xueliang,et al."Relationship between the spatial distribution of landslides and rock mass strength, and implications for the driving mechanism of landslides in tectonically active mountain ranges".ENGINEERING GEOLOGY 292(2021):8.

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来源:地质与地球物理研究所

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