Volume 25 Issue 6
Dec.  2019
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Article Navigation >  Journal of Geomechanics  > 2019  >  25(6): 1048-1057
LI Bing, WANG Jianxin, WANG Xianjun, et al., 2019. DISTRIBUTION OF PRESENT-DAY CRUSTAL STRESS AND TECTONIC ANALYSIS IN THE RONGJIANG CALEDONIAN FOLD BELT, SOUTHEASTERN GUIZHOU. Journal of Geomechanics, 25 (6): 1048-1057. DOI: 10.12090/j.issn.1006-6616.2019.25.06.087
Citation: LI Bing, WANG Jianxin, WANG Xianjun, et al., 2019. DISTRIBUTION OF PRESENT-DAY CRUSTAL STRESS AND TECTONIC ANALYSIS IN THE RONGJIANG CALEDONIAN FOLD BELT, SOUTHEASTERN GUIZHOU. Journal of Geomechanics, 25 (6): 1048-1057. DOI: 10.12090/j.issn.1006-6616.2019.25.06.087
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DISTRIBUTION OF PRESENT-DAY CRUSTAL STRESS AND TECTONIC ANALYSIS IN THE RONGJIANG CALEDONIAN FOLD BELT, SOUTHEASTERN GUIZHOU

doi: 10.12090/j.issn.1006-6616.2019.25.06.087
  • 1.

    Institute of Crustal Dynamics, China Earthquake Administration, Beijing 100085, China

  • 2.

    School of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, Anhui, China

More Information
  • Received: 2019-06-15
  • Revised: 2019-08-29
  • Published: 2019-12-31
    Abstract
  • Southeastern Guizhou is located in the Rongjiang Caledonian fold belt, which is very undeveloped in caprock. In order to find out the state of crustal stress in this area, the hydraulic fracturing stress measurements of 7 boreholes were carried out. A comparative study was made on the distribution differences of crustal stress in the southeast, west and northwest of southeastern Guizhou, combining with the research results of west Guizhou and crustal measurement data of a borehole in northwestern Guizhou. Finally the fault stability around the sampling borehole area was discussed in association with fault activities and the Byerlee criterion. The results demonstrate that the horizontal principle stress is dominant in the study area, and the maximum horizontal principal stress is in the N-W direction; according to the Anderson fault theory, the relative magnitude of the three-direction principal stress is favorable to the movement of the thrust fault and strike-slip fault, which corresponds to the nature of the active fault developed in the study area; the linear fitting results of the maximum and minimum horizontal principal stresses show that the gradient of horizontal principal stress is larger than that of the coal seam area in western Guizhou, the northeastern Guangxi basin and the whole country, and the maximum horizontal principal stress is larger than that of western Guizhou, northwesternern Guizhou and the northeastern Guangxi basin at the similar depth; there are high tectonic stresses near the Sandu fault zone, and the μm value (the ratio of the maximum shear stress to the average principal stress) is higher, which indicates that the fault is in the state of friction limit equilibrium; the tectonic action on both sides of the Sanjiang-Rongan fault is obviously different, and the tectonic action on the west side is stronger than that on the east side; although μm values are high in some boreholes, the direction of regional stresses intersect with the fault at a larger angle, so the fault is stable, which is consistent with the seismicity in the study area.

     

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