The progress of the fault conduit system,include the migration pathway inside a fragile fault zone consists of associated fractures,the fault rock zone without adhesive power and induced fracture zones.

Multi-f ractal spectrum behaviour of fault system and its application;

Fractal characteristics and reservoir distribution of fault system in the northwest margin of Jungar basin;

It is vertically divided into the deep fault system and the shallow fault system bounded by the bottom of Jurassic.

The complicated fracture systems and tectonic framework were formed in the central and southern parts of the South China Sea due to the reciprocal movement of the plates like the Euro-Asia Plate, the Pacific-Philippine Plate and the India-Australia Plate during Mesozoic and Cenozoic.