Experiments on uniaxial and triaxial rock mechanics and rock acoustic emissions have been conducted for research on the impact of rock anisotropy on the development of the fractures of different directions by taking as an example the ultra-low-permeability sandstone reservoir in the Upper Triassic Yanchang Formation within the Ordos Basin.The experimental results prove the existence of anisotropy of the rock mechanical property in the different directions on the plane,which is the chief reason for the production of impacts on the development of different assemblages of fractures in the geological periods.The rock anisotropy usually restricts the development of one assemblage of conjugate shear fractures.The fractures in the Yanchang Formation within the Ordos Basin are mainly shear fractures that formed under two tectonic actions.Theoretically,here,four assemblages of shear fractures should have developed,but due to the effect of a strong rock anisotropy,in each period one assemblage of fractures chiefly developed.Thus,two assemblages of fractures are usually developed in every part at present. Experiments on uniaxial and triaxial rock mechanics and rock acoustic emissions have been conducted for research on the impact of rock anisotropy on the development of the fractures of different directions by taking as an example the ultra-low-permeability sandstone reservoir in the Upper Triassic Yanchang Formation within the Ordos Basin. The experimental results prove the existence of anisotropy of the rock mechanical property in the different directions on the plane, which is the chief reason for for the production of impacts on the development of different assemblages of fractures in the geological periods.s. rock anisotropy usually restricts the development of one assemblage of conjugate shear fractures. the fractures in the Yanchang Formation within the Ordos Basin are mainly under shear fractures that formed under two tectonic actions.Theoretically, here, four assemblages of shear fractures should have developed, but due to the effect of a strong rock anisotropy, in each period one assemblage o f fractures chiefly developed.Thus, two assemblages of fractures are usually developed in every part at present.