摘要
Kongnan area of Huanghua depression has experienced rift stage, faulted-sag stage and sag stage with complex fault systems. Based on the activity, the fault systems can be divided into two types: The Cangdong extension fault system and Xuxi right-lateral strike-slip fault system. Cangdong fault is a listric normal fault slipping into the deep crust and controlling the global deformation of Kongnan area. The Xuxi fault can be considered as a secondary fault in the hanging wall of Cangdong fault. With the control of the process of extension and strike-slip, abundant hydrocarbon had accumulated in the central-north part of Kongnan area.