临清地区自三叠纪末—侏罗纪经历了拉张—挤压—拉张的交替更迭的地洼发展阶段。由于受边界条件的影响,控制两个地洼盆地发展期构造活动是多因素的,在盆地内形成的构造期也因地而异,故其内部构造显得十分复杂。两套地洼型含油气建造的存在,也因构造型相的差别,使其各凹陷的含油气性呈现出较大的级别差异 Since the end of the Triassic, the Jurassic experienced a stage of development of depression in the Linqing area. Due to the influence of the boundary conditions, controlling the tectonic activities during the development of the two diwako basins is multi-factor, and the tectonic period formed in the basin varies from place to place. Therefore, its internal structure is very complicated. The existence of two sets of subsurface oil-bearing gas reservoirs also caused a great difference in oil-gas content in each depression due to the differences in tectonic facies