青藏高原构造变形圈-岩体松动圈-地表冻融圈-工程扰动圈互馈灾害效应

彭建兵; 张永双; 黄达; 王飞永; 王祚鹏

doi:10.3799/dqkx.2023.137

Volume 48 Issue 8

Aug. 2023

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Article Navigation > Earth Science > 2023 > 48(8): 3099-3114

Peng Jianbing, Zhang Yongshuang, Huang Da, Wang Feiyong, Wang Zuopeng, 2023. Interaction Disaster Effects of the Tectonic Deformation Sphere, Rock Mass Loosening Sphere, Surface Freeze-Thaw Sphere and Engineering Disturbance Sphere on the Tibetan Plateau. Earth Science, 48(8): 3099-3114. doi: 10.3799/dqkx.2023.137

Citation:

Peng Jianbing, Zhang Yongshuang, Huang Da, Wang Feiyong, Wang Zuopeng, 2023. Interaction Disaster Effects of the Tectonic Deformation Sphere, Rock Mass Loosening Sphere, Surface Freeze-Thaw Sphere and Engineering Disturbance Sphere on the Tibetan Plateau. Earth Science, 48(8): 3099-3114. doi: 10.3799/dqkx.2023.137

Citation:

Peng Jianbing, Zhang Yongshuang, Huang Da, Wang Feiyong, Wang Zuopeng, 2023. Interaction Disaster Effects of the Tectonic Deformation Sphere, Rock Mass Loosening Sphere, Surface Freeze-Thaw Sphere and Engineering Disturbance Sphere on the Tibetan Plateau. Earth Science, 48(8): 3099-3114. doi: 10.3799/dqkx.2023.137

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Interaction Disaster Effects of the Tectonic Deformation Sphere, Rock Mass Loosening Sphere, Surface Freeze-Thaw Sphere and Engineering Disturbance Sphere on the Tibetan Plateau

doi: 10.3799/dqkx.2023.137

Peng Jianbing^{1, 2, 3
,},
Zhang Yongshuang^{1, 2},
Huang Da³,
Wang Feiyong^{1, 2},
Wang Zuopeng^{1, 2}

1.
Institute of Geosafety, China University of Geosciences, Beijing, 100083, China
2.
Engineering and Technology Innovation Center for Geosafety Risk Prevention and Control of Major Projects, MNR, Beijing 100083, China
3.
College of Geological Engineering and Geomatics, Chang'an University, Xi'an 710054, China

Received Date: 2023-05-01
Publish Date: 2023-08-25

Abstract

Abstract

The essence of intense collision and continuous deformation of the Tibetan Plateau plate is the effect of the earth's sphere. It is also the key to explore the relationship of continuous tectonic deformation and shallow response, and catastrophe-pregnant mechanism. Based on the analyses of the dynamic background of sphere action on the Tibetan Plateau, this paper, from the perspective of engineering geology, divides the key zone of shallow crust into four types of the sphere, including tectonic deformation sphere, rock mass loosening sphere, surface freeze-thaw sphere, and engineering disturbance sphere. Meanwhile, this paper studies the deformation and failure law of rock-soil mass, the stability state and engineering safety of the rock-soil mass, as well as the behavior and mechanism of disaster in various spheres. This study shows that the mutual feedback of the four types of sphere has a profound impact on the geological body stability and disaster dynamic mechanism at different scales; that is, plate tectonic dynamic forms the tectonic deformation sphere, restricting the stability of regional geological body, and controlling the disaster-pregnant process; uplift dynamic of the plateau forms the rock mass loosening sphere, restricting the stability of engineering geological body, and controlling the formation of disasters; climatic change dynamic forms the surface freeze-thaw sphere, restricting the stability of engineering rock-soil mass, and controlling the evolution of disaster chains; human engineering force forms the engineering disturbance sphere, restricting the stability of engineering structures, and controlling the occurrence of engineering disasters. The lower sphere is inclusive of the upper sphere, and there is a progressive evolution law from bottom to top, which makes the rock-soil mass structure more complex, and the engineering geological problems and disaster effects more significant. This study provides a novel research idea for the geological safety risk prevention of major engineering construction.
- Tibetan Plateau,
- sphere interaction,
- disaster effect,
- major project,
- geosafety,
- engineering geology

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References(102)

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Interaction Disaster Effects of the Tectonic Deformation Sphere, Rock Mass Loosening Sphere, Surface Freeze-Thaw Sphere and Engineering Disturbance Sphere on the Tibetan Plateau

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