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现代地质 ›› 2007, Vol. 21 ›› Issue (Suppl): 58-62.

• 地质资源 • 上一篇    下一篇

渤海湾盆地沾化凹陷古近系沙二上亚段砂岩储层成岩相研究

张鹏飞,陈世悦,张明军,鄢继华   

  1. 中国石油大学 地球资源与信息学院,山东 东营257061
  • 收稿日期:2006-10-20 修回日期:2006-11-22 出版日期:2007-08-20 发布日期:2007-08-20
  • 作者简介:张鹏飞,男,博士研究生,1981年出生,矿物学、岩石学、矿床学专业,主要从事沉积学及岩相古地理研究。
  • 基金资助:

    国家“十五”重大科技攻关项目(2001BA605A09)

AThe Study of Diagenetic Facies of Sandstone Reservoirs of Upper Es2 of Paleogene in Zhanhua Sag,Bohai Bay Basin

ZHANG Peng-fei, CHEN Shi-yue, ZHANG Ming-jun, YAN Ji-hua   

  1. College of Georesources and Information, China University of Petroleum, Dongying, Shandong257061,China
  • Received:2006-10-20 Revised:2006-11-22 Online:2007-08-20 Published:2007-08-20

摘要:

沾化凹陷是渤海湾盆地济阳坳陷中的一个次级构造单元。为了更精确地预测沾化凹陷沙二上亚段砂岩储层的分布及内部储集性能的差异,该项研究以84口探井的岩心、录井、测井、地震、普通薄片、铸体薄片、储层物性等资料为基础,对研究区砂岩储层的沉积及成岩演化特征进行了系统的研究。储层主要发育于三角洲、扇三角洲沉积体系的水下分流河道、河口坝以及滨浅湖滩坝内。储层的岩性主要为岩屑石英砂岩和岩屑砂岩,储集空间以原生孔隙为主,部分地区次生溶孔发育,储层孔隙度主要集中在8%~24%之间,渗透率在1×10-3~100×10-3μm2之间。应用成岩相的理论和聚类分析方法将储层划分为3种成岩相:Ⅰ.弱压实粘土环边胶结成岩相;Ⅱ.中压实残余粒间孔成岩相;Ⅲ. 强压实碳酸盐溶蚀成岩相。阐述了各种相的特征,并且完成了成岩相的平面分布图。

关键词: 储层, 成岩相, 沾化凹陷, 沙二上亚段

Abstract:

Zhanhua sag is the sub-tectonic unit of the Jiyang depression in Bohaiwan Basin. In order to find out the regularities of distribution and the characteristics of the reservoir in Upper Es2 of the Zhanhua sag, based on the data of the core,well-logging,seism,thin-section and the physical property in 84 wells, the characteristics of the sedimentary and diagenetic evolution of the reservoir are studied systemically. The reservoir primarily appeared in some microfacies, such as the fan-delta subaqueous distributary channel, mouth bar, beach-bar in the littoral and shallow lake. The reservoir is primarily lithoclastic quartz sandstone and lithic sandstone; the pore is chiefly primary pore;and the porosity and permeability of the reservoir are between 8% and 24%, 1×10-3μm2and 100×10-3μm2 respectively. Applying the theory of the diagenetic facies and cluster methods, the reservoir is classified into three types, which are respectively weak compaction and clay cementation, middle compaction, strong compaction and solution. Based on the analysis of the characteristics of three facies, the distribution ichnography of the diagenetic facies is completed.

Key words: reservoir, diagenetic facies,  , Zhanhua sag, Upper Es2

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