Volume 24 Issue 1
Feb.  2018
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Article Navigation >  Journal of Geomechanics  > 2018  >  24(1): 25-34
NIU Linlin, FENG Chengjun, ZHANG Peng, et al., 2018. IN-SITU MEASUREMENTS IN THE SOUTHERN MARGIN OF THE ORDOS BLOCK. Journal of Geomechanics, 24 (1): 25-34. DOI: 10.12090/j.issn.1006-6616.2018.24.01.003
Citation: NIU Linlin, FENG Chengjun, ZHANG Peng, et al., 2018. IN-SITU MEASUREMENTS IN THE SOUTHERN MARGIN OF THE ORDOS BLOCK. Journal of Geomechanics, 24 (1): 25-34. DOI: 10.12090/j.issn.1006-6616.2018.24.01.003
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IN-SITU MEASUREMENTS IN THE SOUTHERN MARGIN OF THE ORDOS BLOCK

doi: 10.12090/j.issn.1006-6616.2018.24.01.003
  • 1.

    Institute of Geomechanics, Chinese Academy of Geological Sciences, Beijing 100081, China

  • 2.

    Key Laboratory of Neotectonic Movement & Geohazard, Ministry of Land and Resources, Beijing 100081, China

More Information
  • Received: 2017-11-20
  • Revised: 2017-12-05
  • Published: 2018-02-01
    Abstract
  • The crustal stress distribution pattern and fault activity of the shallow crust in the southern margin of the Ordos block are studied by using the stress test data obtained from hydraulic fracturing method. The results reveal that the maximum and minimum horizontal principal stress show a good linear relationship with depth. The gradient is 0.032 and 0.021, respectively. Stress structure of SH > Sh > SV is favorable for the activity of the reverse fault and that is different from the normal fault occurred in the 1556 Huashan earthquake. The direction of the maximum horizontal principal stress is NS-NNW, which is consistent with the direction of velocity vector field. It is different from regional tectonic stress direction interpreted by other data, which may be affected by the fault activity around the Ordos block. The crustal activity in the study area is discussed by using the Mohr-Coulomb criterion and Byerlee's law under the premise that the friction coefficient is 0.6~1.0. We found that the measured points in the southern margin of Ordos block have not reached or exceeded the limit of the earth's crust rupture and there are no fault instability or earthquake and other forms of the activities, which is in a relatively stable state of crustal stress. New in-situ stress measurement data have been added to the area. The research results provide the boundary conditions for the engineering design and construction, numerical simulation of tectonic stress field in the area, which is of great significance for the study of geological hazard assessment, crustal stability and continental dynamics.

     

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