台北凹陷西部七克台组自生、自储、自盖,构成良好的区域性生储盖组合.
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Cretaceous sandstone and Eogene mudstone are the main reservoir and caprock.
油气从油气田东部注入,由东向西运移并差异聚集,依次形成凝析气藏、带油环凝析气藏和挥发性油藏.
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Finally, a method of estimating displacement pressure of caprock is presented.
提出了盖层排替压力的求取方法.
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研究了源盖层浓度封闭作用形成条件及封闭机理.
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