摘要
In the paper, the growth index and fault throw of different trends in the Linyi fracture belt have been studied. The sedimentation characteristics for each sedimentary subzone of ES4 and ES3 have been analyzed. The episodic activities of fault are found to control stratigraphic sedimentary and spatial distribution, which makes subsiding center migrate from west to east along the direction of the fracture belt. Furthermore, the contraposition relation between the development characteristics and lithology of faulted uplifted wall and downthrow block have also been detailedly discussed and the migration track of oil and gas and potential zones for exploration in the Linyi fracture belt have been redefined. The research is helpful for the exploration and development of the Huimin Depression.