Scientific Reports (May 2024)

Determination of mine fault activation degree and the division of tectonic stress hazard zones

  • Tianwei Lan,
  • Yonghao Liu,
  • Yongnian Yuan,
  • Ping Fang,
  • Xiangdong Ling,
  • Chuang Zhang,
  • Yabin Li,
  • Yang Li,
  • Wei Feng

DOI
https://doi.org/10.1038/s41598-024-63352-w
Journal volume & issue
Vol. 14, no. 1
pp. 1 – 15

Abstract

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Abstract This article conducts a comprehensive study on the activation characteristics of faults in the mine and analyzes the distribution patterns of the original rock stress field. Through quantitative research and analysis, we determine the partitioning characteristics of tectonic stress in the mine field under the dual effects of fault activation and original rock stress. The study also reveals the significant impact of different fault activation characteristics and different tectonic stress partitions on the stability of roadway surrounding rock. Using the Mohr–Coulomb strength criterion as a foundation, we investigate the mechanisms of fault activation and establish a mathematical model for fuzzy comprehensive evaluation. This model enables us to determine the strength level of fault activation in coal seam 9 of the Limin coal mine and construct a geological structure model. It has realized the transformation of fault activation degree from qualitative evaluation to quantitative evaluation. The stress state analysis software is used to draw the division of tectonic stress dangerous areas under the synergistic effect of fault activation and original rock stress. We then analyze the impact on the stability of roadway surrounding rock in these different hazardous areas. Utilizing the fuzzy comprehensive evaluation method, we take into account the impact of faults on the distribution characteristics of stress fields and the stability of roadway surrounding rock. This approach enables us to more accurately and comprehensively determine the hazardous areas of tectonic stress in the mine field under the dual effects of faults and original rock stress.