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孔店组和沙四段在惠民、东营凹陷是重要的含油气层位，其构造演化可划分为4个阶段，即孔店－沙四期伸展半地堑充填阶段、沙二－沙三期断块强烈活动阶段、沙－东营期断块活动复杂化阶段和晚第三纪－第四纪埋深加大阶段。与此对应孔店组－沙四段中断层的演化序列为板式→铲式→坡坪式；断陷构造样式的演变序列为旋转半地堑→滚动半地堑→复式半地堑。惠民凹陷孔店－沙四期伸展强度最大，东营凹陷沙二、沙三期伸展强度最大。受构造影响，形成沙河街组四段好的烃源岩，且惠民凹陷比东营凹陷更发育。与孔店组和沙河街组四段有关发育二个正常式生储盖组合。断层是主要的运移通道。构造圈闭主要是与断层有关的断块和断鼻。凹中隆地区和边缘斜坡地区是油气成藏的最有利部位。
The Kongdian Formation and Shasi Section are important petroliferous reservoirs in the Huimin and Dongying sags. Their tectonic evolution can be divided into four stages, that is, the Kongdian-Sha4 stretch semi-graben filling stage, the Sha2-Sha3 fault block In the intense activity phase, the complex activities of the Sha-Dongying fault block activity and the late Tertiary-Quaternary burial depth increase stage. Correspondingly, the evolution sequence of the Kongdian-Sha-4 Member fault is plate → shovel-slope type; the evolution sequence of fault tectonic style is rotary semi-grazing → rolling semi-grazing → complex semi-graben. Huimin Depression Kong shop - Sha 4 stretch the greatest strength, Dongying Sag Sand II, Sha 3 maximum extension strength. Affected by tectonics, a good source rock is formed in the fourth member of Shahejie Formation, and the Huimin Depression is more developed than Dongying Depression. And the hole shop group and Shahejie Formation four paragraphs related to the development of two normal type of storage and cover combination. Fault is the main migration channel. Structural traps are mainly fault-related fault blocks and broken nose. The concave Neutral and marginal slopes are the most favorable sites for hydrocarbon accumulation.