摘要
The thrust structures referred as all kinds of traps are located in the lower layer of the thrust fault or the down-thrown of thrust block and consist of three parts of the thrust fault,overlying rock series and underlying rock series. The origins of the thrust structures are the fault-thrust movement by extrusion force and the fault-gliding movement by extensional regime. The thrust structures are widely developed in different tectonic units of various areas in the world. Especially, there are good pool-formed conditions such as hydrocarbon generation, reservoir-cap rock and traps in the thrust structure zone of foreland basins.