“…Extensive compression tests have been put forward to explore the strength and failure features of various anisotropic rock masses at uniaxial and triaxial compression conditions in the laboratory, e.g., slate [ 18 , 19 , 20 ], schist [ 13 , 20 , 21 , 22 , 23 , 24 ], phyllite [ 13 , 25 ], marble [ 13 , 23 ], sandstone [ 3 ], shale [ 26 , 27 , 28 ], limestone [ 28 , 29 , 30 ], mudrock [ 31 ], columnar basalt [ 32 ], and artificially anisotropic rock specimens [ 3 , 33 ]. Numerical studies have also been conducted to investigate the mechanical behavior of anisotropic rock mass intrinsically [ 12 , 34 ]. These effective studies reflect that the deformation and strength properties are largely dominated by the angle between the normal anisotropic structural plane and the direction of minimum principal stress ( ).…”