The cenozoic fault system of southeastern Tarim basin can be divided into three systems:the Altun fault system,Che\'erchen fault system and the West Kunlun fault system.

The East Kunlun Fault zone in Northern Tibetan Plateau is a typical active fault zone,characterized by sinistral strike-slip faults.

Numeric Simulation on Destructive Effect of Golmud-Lhasa Railway Resulting in Stick-Slip Movement of the Eastern Kunlun Fault;

For this event, some researchers have developed an analysis method of brightness temperature difference inside and outside the Eastern Kunlun Fault, and have drawn an important conclusion.

Finite difference numerical simulation of trapped waves in the Kunlun fault zone;

Deformation and tectonic evolution of the Karakorum fault, western Tibet;