GEOLOGICAL CHARACTERISTICS OF THE MAIN ACTIVE FAULTS AND EARTHQUAKES IN HUNAN AND HUBEI AREAS, THE MIDDLE REACHES OF THE YANGTZE RIVER

LI Hao-min; WU Zhong-hai; WANG Hao-nan; WANG Guo-sheng

2016 Vol. 22, No. 3

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Article navigation > Journal of Geomechanics > 2016 > 22(3): 478-499

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LI Hao-min, WU Zhong-hai, WANG Hao-nan, WANG Guo-sheng. GEOLOGICAL CHARACTERISTICS OF THE MAIN ACTIVE FAULTS AND EARTHQUAKES IN HUNAN AND HUBEI AREAS, THE MIDDLE REACHES OF THE YANGTZE RIVER[J]. Journal of Geomechanics, 2016, 22(3): 478-499.

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GEOLOGICAL CHARACTERISTICS OF THE MAIN ACTIVE FAULTS AND EARTHQUAKES IN HUNAN AND HUBEI AREAS, THE MIDDLE REACHES OF THE YANGTZE RIVER

1.
College of Science and Resources, China University of Geosciences, Beijing 100083, China
2.
Institude of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China
3.
Neotectonics and Geological hazard Laboratory, Ministry of land and Resources of China, Beijing 100081, China

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Corresponding author: WU Zhong-hai, wzhh4488@sina.com

Received Date: 18 April 2016

Publish Date: 25 September 2016

Abstract

Abstract

In this paper, the predecessors' achievements were collected and combined with the historical and modern seismic data in Hunan and Hubei areas. The major active faults and historical earthquakes in the areas, characteristics of the main active earthquake-controlled fault system (belt), seismic activity and spatial and temporal distribution were summarized. Research results indicate that the trends of major active faults in this region are mainly of NE, NNE and NW. There are 6 main active fault systems from north to south, including NW trending Qinkun fault system, NE trending fault system in the east of Hubei, Jianghan-Dongting basin fault system, NE trending fault system from west Hubei to west Hunan, NE trending fault system in central and south Hunan, and NEE trending fault system in east of Hunan. Quaternary activities of Jianghan-Dongting basin fault system and NW trending Qinkun fault system are more significant. Seismic activity level in the "Two Lakes" area is relatively low, being in the relatively calm period of the third activity period. Combining modern medium-strong earthquakes data with characteristics of China's seismic intensity zoning, we believed that crust is unstable in the east and west boundaries of the south of Jianghan-Dongting basin, the Ezhou-Huanggang-Wuhan area and fault block uplift area in northwestern Hubei, with higher potential earthquake risk, which should be paid more attentions in the planning and construction of the urban agglomeration, protecting river embankment design and construction of major projects.
- middle reaches of Yangtze River /
- Hunan and Hubei region /
- neotectonics /
- active fault /
- seismic activity /
- evaluation of crustal stability

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References

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