generate questions: The Longmen Shan Fault System is situated in the eastern border of the Tibetan Plateau and contains several faults. This earthquake ruptured at least two imbricate structures in Longmen Shan Fault System, i.e. the Beichuan Fault and the Guanxian–Anxian Fault. In the epicentral area, the average slip in Beichuan Fault was about 3.5 metres (11 ft) vertical, 3.5 metres (11 ft) horizontal-parallel to the fault, and 4.8 metres (16 ft) horizontal-perpendicular to the fault. In the area about 30 kilometres (19 mi) northeast of the epicenter, the surface slip on Beichuan Fault was almost purely dextral strike-slip up to about 3 metres (9.8 ft), while the average slip in Guanxian–Anxian Fault was about 2 metres (6 ft 7 in) vertical and 2.3 metres (7 ft 7 in) horizontal.
Where is the Longmenshan Fault located? {sep_token} What is the average slip in the Beichuan Fault? {sep_token} How large was the slip 30 km northeast of the fault? {sep_token} What was the vertical average slip on the Guanxian-Anxian fault? {sep_token} What was the horizontal average slip on the Guanxian-Anxian fault? {sep_token} Where is the Longmen shan fault located? {sep_token} Where are the Beichuan and Guanxian-Anxian Faults? {sep_token} What was the average vertical slip in the Beichaun Fault? {sep_token} What was the horizontal slippage in the Beichuan Fault at the epicenter? {sep_token} What was the horizontal slippage perpendicular to the fault? {sep_token}