天然气地质学

琼东南盆地宝岛北坡断层封闭性与油气运聚关系

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  • 1.中国石油大学(北京),北京 102249;2.中海石油(中国)有限公司湛江分公司,广东 湛江 524057
张新顺(1988-),男,河南濮阳人,硕士研究生,主要从事石油地质研究.E-mail: vvvzxs@126.com.

收稿日期: 2012-08-21

  修回日期: 2012-10-02

  网络出版日期: 2013-04-10

基金资助

国家重大专项子课题“莺琼盆地低品位天然气成藏机制与潜力分析”(编号:2011ZX05023-004-008)资助.

Fault Sealing Capacity and Relationship with Oil-gas Accumulation at Baodao Northern Slope

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  • 1.China University of Petroleum(Beijing),Beijing 102249,China;2.Zhanjiang Branch of CNOOC Limited,Zhanjiang 524057,China

Received date: 2012-08-21

  Revised date: 2012-10-02

  Online published: 2013-04-10

摘要

在对琼东南盆地宝岛北坡最新油气勘探资料分析基础上,通过比对宝岛北坡A区和B区的油气地球化学特征,利用Knipe三角图和断层连通概率法(FOI)综合评判地区断层封闭性,最后结合油气成藏期、断层主要活动期、沉积相等地质特征,分析宝岛北坡断层封闭性对地区油气运聚产生的影响。结果表明:宝岛北坡A区天然气具有重烃含量高、非烃含量低、碳同位素组成轻且凝析油中不含C30-4甲基甾烷和双杜松烷的特征,这与B区有明显区别;研究区内断层主要活动期为三亚组(T50—T60)沉积时期,在晚期的油气运聚高峰期时断层主要是静止的;现今断层具有分段封闭性的特征,深部断层封闭性较差成为沟通烃源岩和储层的良好通道;断层的分段封闭性特征造成了宝岛A区和B区油气不同的运聚方式,从而导致了气藏中油气性质的不同。

本文引用格式

张新顺,黄志龙,范彩伟,吴红烛,徐新德,李美凝 . 琼东南盆地宝岛北坡断层封闭性与油气运聚关系[J]. 天然气地球科学, 2013 , 24(2) : 356 -364 . DOI: 10.11764/j.issn.1672-1926.2013.02.356

Abstract

Based on the newest oil & gas exploration data of Baodao Northern slope in the Qiongdongnan basin,through oil-gas geochemical comparison of area A and area B,the regional fault sealing capacity was evaluated by Knipe triangle map and fault opening index (FOI).Finally combined with the oil-gas accumulation period,stage of fault activity,sedimentary facies and some other geological factors,influence of the fault closure in the northern slope of Baodao on regional oil and gas migration and accumulation was evaluated.The faults connecting source rock with reservoirs are favorable paths for oil & gas vertical migration,and they have segmented sealing capacity.It is the segmented sealing capacity of faults that result in different oil-gas migration and accumulation modes in area A and area B,which is also the reason of the differences properties of the oil-gas in the gas reservoir.The results show that natural gas in area A has high level of heavy hydrocarbon,low level of non-hydrocarbon,light carbon isotope and the gas condensate without dicadinane and 4-methyl-steranes,which is significantly different from the gases in area B.The faults are active mainly during depositional period of Sanya Formation,which means the faults are static at the peak stage of oil-gas migration.

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