兰州黄河阶地演变过程对滑坡活动的控制效应

张泽林; 吴树仁; 唐辉明; 黎志恒; 赵成; 张永军; 王涛

doi:10.3799/dqkx.2015.143

Volume 40 Issue 9

Sep. 2015

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Article Navigation > Earth Science > 2015 > 40(9): 1585-1597

Zhang Zelin, Wu Shuren, Tang Huiming, Li Zhiheng, Zhao Cheng, Zhang Yongjun, Wang Tao, 2015. Control Effect of Evolution Process of the Yellow River Terrace in Lanzhou on Landslide Activity. Earth Science, 40(9): 1585-1597. doi: 10.3799/dqkx.2015.143

Citation:

Zhang Zelin, Wu Shuren, Tang Huiming, Li Zhiheng, Zhao Cheng, Zhang Yongjun, Wang Tao, 2015. Control Effect of Evolution Process of the Yellow River Terrace in Lanzhou on Landslide Activity. Earth Science, 40(9): 1585-1597. doi: 10.3799/dqkx.2015.143

Citation:

Zhang Zelin, Wu Shuren, Tang Huiming, Li Zhiheng, Zhao Cheng, Zhang Yongjun, Wang Tao, 2015. Control Effect of Evolution Process of the Yellow River Terrace in Lanzhou on Landslide Activity. Earth Science, 40(9): 1585-1597. doi: 10.3799/dqkx.2015.143

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Control Effect of Evolution Process of the Yellow River Terrace in Lanzhou on Landslide Activity

doi: 10.3799/dqkx.2015.143

1.
Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
2.
Faculty of Engineering, China University of Geosciences, Wuhan 430074, China
3.
Geological Environmental Monitoring Institute of Gansu Province, Lanzhou 730000, China

Received Date: 2015-03-23
Publish Date: 2015-09-15

Abstract

Abstract

In order to explore the relationship between the geological settings and the development of the slides, and mechanisms of landslides induced by evolution of the Yellow River terrace in Lanzhou, the development phase characters of the Yellow River valley evolution in Lanzhou, control effect of the valley evolution to landslides and landslide formation model are studied in this paper based on extensive analysis of regional engineering geology data, combined with Quaternary geomorphology and engineering geology. It is found that: (1) the control effect of landslides in Lanzhou induced by the Yellow River valley evolution shows phase in time and zonation in space. The landslides have different development modes and formation mechanisms in different phases of river valley evolution. (2) The major inducing factors of terrace landslides are intense neotectonics uplifting, strong incision of the Yellow River and relative moisture paleoclimate during the terraces formed. The weak intercalated layers formed in Tertiary mudstone stratum may induce large scale loess-mudstone landslides while it may develop small-middle scale landslides and collapses in the loess layer. The landslides may lead to the deficiency of partial terraces during the river valley evolution.
- the Yellow River terrace,
- terrace evolution,
- landslide,
- control effect,
- landslide formation and mechanism,
- slope stability,
- engineering geology

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References(37)

References

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Control Effect of Evolution Process of the Yellow River Terrace in Lanzhou on Landslide Activity

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