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WeiWei ZHOU, YongCun FENG, XiaoRong LI, et al., 2025. ZHOU Weiwei, FENG Yongcun, LI Xiaorong, LIU Jie, SU Feiyu, HU Han. Journal of Geomechanics. DOI: 10.12090/j.issn.1006-6616.2025095
Citation: WeiWei ZHOU, YongCun FENG, XiaoRong LI, et al., 2025. ZHOU Weiwei, FENG Yongcun, LI Xiaorong, LIU Jie, SU Feiyu, HU Han. Journal of Geomechanics. DOI: 10.12090/j.issn.1006-6616.2025095

ZHOU Weiwei, FENG Yongcun, LI Xiaorong, LIU Jie, SU Feiyu, HU Han

doi: 10.12090/j.issn.1006-6616.2025095
Funds:  National Science and Technology Major Project(2025ZD1011100)
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  • Received: 2025-07-30
  • Revised: 2025-11-30
  • Accepted: 2025-12-03
  • Available Online: 2025-12-12
  • [Objective] To improve the computational efficiency and accuracy of stress tensor inversion from fault-slip data, and to address the limitations of conventional grid search methods—namely high computational cost and susceptibility to local optima—an inversion approach based on intelligent optimization algorithms was investigated. [Methods and Process] A novel fault-slip data inversion method based on the Quantum-behaved Particle Swarm Optimization (QPSO) algorithm is proposed, in which the stress tensor is parameterized by four variables: three Euler angles (α, β, γ) representing the orientations of the principal stress axes and a shape factor (stress ratio Φ). A misfit function is constructed based on the angular deviation between the shear stress direction and the observed slip vector. To enhance convergence performance, an elite-guided learning strategy was adopted, incorporating a reward-penalty feedback mechanism and a tensor distance metric to quantify stress similarity. Multiple synthetic stress models were tested using a simulated fault-slip dataset, and the inversion performance of QPSO was compared with the conventional grid search method in terms of efficiency and accuracy. [Results] The results demonstrate that the proposed QPSO-based inversion method achieves a non-convergence rate below 8%, with the computational time reduced to approximately 1/27 of that required by the grid search approach. The method converges rapidly in high-dimensional, multimodal parameter spaces and accurately identifies normal, reverse, and strike-slip stress regimes. The clustering of inversion results is well defined, indicating strong stability and physical consistency. [Conclusion] The QPSO-based method exhibits significant advantages in stress tensor inversion from fault-slip data, including high computational efficiency, strong adaptability, and fast convergence. It provides effective technical support for regional paleo-stress field reconstruction and focal mechanism analysis, and offers methodological insights for the integration of intelligent optimization algorithms in geomechanics applications.

     

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