王纯;张研;吴小洲;马晓宇;黄昱丞;宋志慧;

• 1:中国石油勘探开发研究院

摘要(Abstract)：

郯庐断裂带在前古近纪及新生代分别发生左旋走滑和右旋走滑运动,造成辽河滩海地区东部的构造演化过程相对复杂。利用地震资料精细解释、构造分析和储层预测等方法,分析辽河滩海地区东部构造演化过程及潜山油气运聚。结果表明:前古近纪时期NE向左旋走滑的燕南、燕东断层,以及EW向的中—古生代断层形成燕南潜山带的内幕形态,潜山带北部内幕圈闭奥陶系储层厚度大、裂缝发育程度高;始新世时期东部凹陷沉积研究区烃源岩地层;渐新世时期燕南断层右行走滑影响潜山带的平面及纵向形态,并开启油气往潜山内幕圈闭运移的通道。该研究为下辽河—辽东湾地区的潜山勘探提供参考。

关键词(KeyWords)：辽河滩海东部;构造演化;潜山内幕;油气运移

Abstract:

Keywords:

基金项目(Foundation):

作者(Author):王纯;张研;吴小洲;马晓宇;黄昱丞;宋志慧;

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参考文献(References)：

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