ISSN 1006-3021 CN11-3474/P
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山西盆地现今地应力状态与地震危险性分析
  
关键词:Shanxi basin  hydraulic fracturing  in situ stress measurement  stress state  Coulomb faulting criterion
基金项目:深部探测技术与实验研究专项项目(编号: SinoProbe-06);公益性行业科研费专项项目(编号: 200811070)
作者单位E-mail
陈群策 国土资源部新构造运动与地质灾害重点实验室中国地质科学院地质力学研究所 chenqunce@sina.com 
安其美 中国地震局地壳应力研究所  
孙东生 国土资源部新构造运动与地质灾害重点实验室中国地质科学院地质力学研究所  
杜建军 国土资源部新构造运动与地质灾害重点实验室中国地质科学院地质力学研究所  
毛吉震 中国地震局地壳应力研究所  
丰成君 国土资源部新构造运动与地质灾害重点实验室中国地质科学院地质力学研究所  
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摘要:
Current In-situ Stress State of Shanxi Basin and Analysis of Earthquake Risk
      Hydraulic fracturing in-situ stress measurements were carried out in 13 boreholes in the southern and northern parts of Shangxi Basin, and the magnitude and direction as well as the distribution regularity of the stress values were obtained. In Wutaishan and Yanmenguan areas within the northern part of Shanxi basin, the magnitude of the measured maximum horizontal principal stress is 8~12 MPa in the depth range of 400~600 m. In Linfen and Yuncheng areas within the southern part of Shanxi basin, the tectonic stress is much higher, with the measured maximum horizontal principal stress being 20~28 Mpa in the depth range of 400~500 m. Obviously, the magnitude of the stress in the southern part is much higher than that in the northern part. According to Coulomb faulting criterion and by using the above in-situ stress data, the authors studied the characteristics and activities of the faults in the study area. The results show that in Wutai, Yanmenguan and Linfen, the stress values have not reached the critical value, whereas in Yuncheng area, the values have reached the lower limit of the fault activity; moreover, if the pore pressure is taken into account, the maximum horizontal principal stress has reached the critical value for reverse fault activity, and the strain accumulation is even much higher. It is suggested that much more attention should be paid to this area.
CHEN Qun-ce,AN Qi-mei,SUN Dong-sheng,DU Jian-jun,MAO Ji-zhen,FENG Cheng-jun.2010.Current In-situ Stress State of Shanxi Basin and Analysis of Earthquake Risk[J].Acta Geoscientica Sinica,31(4):541-548.
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