摘要
Negative structural belt is one of the key areas of hidden reservoir exploration.Depression contains abundant hydrocarbon resources.But it is difficult for exploration due to the geological characters of low structural position,deep buried reservoir and complex accumulation types.In this paper,through analyzing structural features,distribution in the reservoir,reservoir-forming conditions,regularities of distribution and other aspects of Penglaizhen formation in western Sichuan-Deyang,we make an in-depth evaluation on hydrocarbon enrich major control factors and its regularities of distribution of this negative structural belt,thus making a conclusion that hidden reservoir in negative structural belt is controlled by porosity sand body which connects to or is adjacent to source rock fault,by effective lithologic trap,by boundary fault of communication source rocks,and by paleostructual position where lithologic trap has stayed during accumulation stages.These points of views held in this paper possess important significance in electing advantageous exploratory area in negative structural belt in western Sichuan depression and in identifying potential exploration targets.