Study on the mechanism of disparate fault activation responses during coal seam mining affected by upper goaf: a comparative study based on the advancement of the upper and lower plates
Abstract Fault activation serves as a key mechanical mechanism inducing dynamic hazards such as rockbursts and mine tremors during deep coal seam mining. Its evolution is significantly influenced by disturbances from overlying goaf areas and the advancement method of the working face. Taking the F17 normal fault in the South 2 Lower Mining Area of Dongrong No. 2 Mine as the engineering context, a three-dimensional numerical model was constructed under the condition of an existing upper 16# coal seam goaf. Comparative analysis was conducted for two working face advancement scenarios along the fault’s hanging wall and footwall in the 17# coal seam. The evolution characteristics of fault stability were characterized using the ratio of shear stress to normal stress on the fault plane. Results indicate that the upper goaf significantly reduces normal stress on the fault’s hanging wall, triggering shear response within approximately 20–40 m of the working face. Under upper-plate advancement conditions, the shear stress/normal stress ratio gradually increases and stabilizes within the 0.20–0.25 range, with fault activation manifesting as progressive slip and a maximum relative displacement of approximately 120 mm. During the lower plate advance, shear stress rapidly concentrates, causing the shear stress/normal stress ratio at the fault plane to exceed 0.25. Fault slip exhibits sudden intensification, with a significantly larger affected area and higher intensity compared to the upper plate advance. Research indicates that the combined effects of the weakening influence of the goaf and the superposition of mining-induced stresses jointly govern the asymmetric evolution of fault activation. Specifically, the upper plate advance is primarily characterized by gradual activation, whereas the lower plate advance is prone to inducing sudden instability.
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