The Major Controlling Factors Analysis of Hydrocarbon Accumulation on the Gentle Slope Belt of the Southeastern Liaodong Bay Depression

Yongjun Liu, Xiang-yang Tu, Wensen Zhu, Geng Qian, De-bing Zhang
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Abstract

Oil and gas discovery in the Liaodong Bay Depression is mainly distributed in the steep slope, the uplift and the sag zone at current situation. The reservoir developed on southeastern gentle slope zone is the first discovery in this area, which has great significance to the study of the gentle slope zone hydrocarbon accumulation regularity. Based on the analysis of the hydrocarbon accumulation condition of the gentle slope zone, the major controlling factors and hydrocarbon accumulation pattern of the gentle slope zone are summarized. It shows that the gentle slope belt has the superior accumulation conditions, where develops Lithological-tectonics traps and lithological traps Controlled by fracture and provenance. The source rock circumstance is advantageous too, because the gentle slope zone is close to the hydrocarbon-rich Liaozhong sag. The mudstone in Dongying formation(Ed) and the first section of Shahejie formation (Es1) and the sandstone in the second member of Shahejie formation (Es2) are form into a good reservoir cap association. Hydrocarbon accumulation in the gentle slope belt is mainly controlled by 3 factors: the development of the reservoirs in the Es2 is controlled by the valley-slope break coupling; the migration of oil and gas is controlled by “Fault-unconformity-sandbody”(FUS) long-range efficient migration system; reservoir physical properties and oil and gas test capacity are controlled by sedimentary facies differences. There are two reservoir models: lithology - tectonics and lithology.
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辽东湾坳陷东南部缓坡带油气成藏主控因素分析
目前辽东湾坳陷油气发现主要分布在陡坡带、隆起带和凹陷带。东南缓坡带上发育的储层是本区首次发现,对研究缓坡带油气成藏规律具有重要意义。在分析缓坡带油气成藏条件的基础上,总结了缓坡带油气成藏主控因素和成藏模式。表明缓坡带具有优越的成藏条件,发育岩性构造圈闭和受断裂和物源控制的岩性圈闭。缓坡带靠近油气富集的辽中凹陷,烃源岩环境有利。东营组和沙一段泥岩与沙二段砂岩形成良好的储盖组合。缓坡带油气成藏主要受3个因素控制:沙二段储层发育受谷-坡断裂耦合控制;油气运移受“断裂-不整合-砂体”(FUS)远程高效运移系统控制;储层物性和油气测试能力受沉积相差异的控制。有两种储层模式:岩性-构造型和岩性型。
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