ACTIVITY STUDY AND DISASTER EFFECT ANALYSIS OF THE NORTH SECTION OF HUANGZHUANG-GAOLIYING FAULT IN BEIJING

ZHANG Lei; ZHANG Xiaoliang; BAI Lingyan; YANG Tianshui; CAI Xiangmin; LIANG Yanan

2017 Vol. 23, No. 4

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ZHANG Lei, ZHANG Xiaoliang, BAI Lingyan, YANG Tianshui, CAI Xiangmin, LIANG Yanan. ACTIVITY STUDY AND DISASTER EFFECT ANALYSIS OF THE NORTH SECTION OF HUANGZHUANG-GAOLIYING FAULT IN BEIJING[J]. Journal of Geomechanics, 2017, 23(4): 548-557.

Citation:

ACTIVITY STUDY AND DISASTER EFFECT ANALYSIS OF THE NORTH SECTION OF HUANGZHUANG-GAOLIYING FAULT IN BEIJING

1.
Beijing Institute of Geological Survey, Beijing 100195, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Beijing 100083, China

Received Date: 06 January 2017

Publish Date: 25 August 2017

Abstract

Abstract

In order to further study the Huangzhuang-Gaoliying hidden active fault in the innovation industrial site, future technology city of Beijing, the structural characteristics of the fault zone, Quaternary activity as well as disaster-causing mechanism were determined by the shallow artificial earthquake, high-density resistivity method and drilling engineering. The results show that the north section of the Huangzhuang-Gaoling fault presents as a tensional normal fault in general and dips 70°—80° SE. Near the bedrock depth the vertical separation is relatively large. The fault extending up to the inside of the Quaternary system has the characteristics of listric fault and its occurrence gradually becomes stepper. Parts of the fault are combined with feature "Y" shape. The north section of Huangzhuang-Gaoliying fault has been active since Quaternary, and the average vertical velocities were respectively 0.07 mm/a, 0.04 mm/a, 0.23 mm/a, and 0.10 mm/a in early Pleistocene, middle Pleistocene, late Pleistocene and Holocene. The change characteristics are consistent with that of the neotectonics of Xishan uplift. There has been a strong creeping deformation in the Huangzhuang-Gaoliying fault since Holocene. As the lower walls of the fault keep moving, the geological disasters, such as ground fissures, ground subsidence, wall cracking and so on, were formed along the fault zone.
- active fault /
- Huangzhuang-Gaoliying fault /
- velocity /
- geological disaster /
- Quaternary

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References

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