摘要
介绍了挪威埃科菲斯克油田的基本概况及油田勘探历史,描述了该盆地的演化、油气系统、区域地层及沉积相。该油田的构造类型为盐丘构造,主要的储集层为麦斯特里希特统(K2)—下古新统(丹麦阶)托尔组和埃科菲斯克组。埃科菲斯克组以构造裂隙为主,托尔组主要发育与缝合线有关的裂隙。白垩地层主要为生物成因,其成分为分解的贝壳或浮游的Cocccophorid藻颗石、浮游类和海底有孔虫类。
The Norwegian Ekofisk Oilfield was introduced in detail covering the exploration history, basin evolution, petroleum systems, regional stratigraphy and depositional facies. Oil is trapped within an elongate saltcored dome mainly by four-way dip closure. The principal reservoirs are the Tor and Ekofisk formations of Maastrichtian-Lower Paleocene (Danian) age. Tectonic fractures are the most common type in the Ekofisk Formation, whereas stylolite-associated fractures dominate in the Tor Formation and have greatly enhanced reservoir connectivity. The principal biogenic components of chalk are the disaggregated tests or coccoliths of planktonic coccophorid algae and planktonic and benthonic foraminifera.
出处
《海相油气地质》
2005年第1期49-60,共12页
Marine Origin Petroleum Geology