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在综合前人研究成果的基础上 ,认为造山楔进作用是前陆盆地与造山带耦合的主要动力学机制 ;冲断作用控制沉积物的分布和扩散型式 ;滑脱褶皱、断弯褶皱和断展褶皱是耦合过程中产生的主要变形样式 ;前陆盆地油气藏的分布特征受耦合过程影响的圈闭展布特征的控制。在靠近冲断带一侧或冲断带内 ,主要是背斜油气藏 ;在靠近克拉通一侧 ,以地层油气藏为主 ;在两者之间则形成岩性油气藏。
On the basis of the previous research results, it is considered that the orogenic wedge action is the main dynamic mechanism of the coupling between the foreland basin and the orogenic belt; the thrust distribution controls the distribution and diffusion patterns of sediments; the extensional fold, bend bend fold and discontinuity Folds are the major deformation patterns during the coupling process. The distribution characteristics of the foreland basin are controlled by the characteristics of the trap distribution influenced by the coupling process. Near the side of the thrust belt or thrust belt, there are mainly anticlinal reservoirs; on the side close to the craton, the stratigraphic reservoirs are predominant; lithologic reservoirs are formed between the two.