金湖凹陷铜城断裂带阜宁组低渗储层成因研究
Inner Mongolia Petrochemical Industry(2010)
Abstract
金湖凹陷铜城断裂带为龙岗次凹、汊涧次凹之间的隆起带,构造发育,是油气聚集的有利区带。但阜宁组砂岩储集层物性差,埋藏较深,为低孔低渗储层。通过对该区沉积相、砂体展布、储层储集特征、构造特征的研究,加深了对该区地质规律的认识,提出了该区北部是下步勘探的有利区。
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