“…In most cases, the fault zone is a weak zone with low strength, deformability, high water permeability and poor water resistance, and the physical and mechanical properties of the rock mass on both sides of the fault are significantly different (Liu, et al, 2010). A roadway crosses the fault zone where the geological conditions are complex and abrupt (Islam and Shinjo, 2009), the surrounding rock has asymmetric large deformation and failure under the influence of high stress, fault and fracture cutting, which makes the deep roadway support problem more serious (Wang, et al, 2000;He, et al,2011).…”