The Wenchuan MS8.0 earthquake occurred on the Longmenshan fault which inclines at a dip angle exceeding 60 degrees.Since most thrust earthquakes occur on faults with dip angles of about 30 degrees,it is enigmatic why the Wenchuan earthquake occurred on such a steep fault.In this study we use a simple finite element model to investigate how the stress state in the fault changes with the variation of Poisson’s ratio.The results show that,with the Poisson’s ratio in the fault increasing,the magnitudes of the principal stresses increase and the maximum shear stress decrease,and,especially,the angle between the maximum principal stress and the fault plane decreases,which will enhance the driving force to overcome the frictional resistance on the fault.The increase of Poisson’s ratio in the fault may be an important factor to affect the occurrence of the fault earthquakes with large angles between maximum principal stress and fault plane. The Wenchuan MS8.0 terror occurred on the Longmenshan fault which inclines at a dip angle exceeding 60 degrees .ince most thrust earthquakes occur on faults with dip angles of about 30 degrees, it is enigmatic why the Wenchuan earthquake occurred such such a steep fault. In this study we use a simple finite element model to investigate how the stress state in the fault changes with the variation of the variation of Poisson’s ratio. Results show that, with the Poisson’s ratio in the fault increasing, the magnitudes of the principal stresses increase and the maximum shear stress decrease, and, especially, the angle between the maximum principal stress and the fault plane decreases, which will enhance the driving force to overcome the frictional resistance on the fault. The increase of Poisson’s ratio in the fault may be an important factor to affect the occurrence of the fault earthquakes with large angles between maximum principal stress and fault plane.