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现代地质 ›› 2013, Vol. 27 ›› Issue (5): 1089-1098.

• 油气成藏条件 • 上一篇    下一篇

东营凹陷沙河街组储层高岭石分布特征及其影响因素

郭佳1,2,曾溅辉1,2,宋国奇3,张永旺1,2,王学军4,孟伟1,2   

  1. 中国石油大学(北京)油气资源与探测国家重点实验室,北京 102249
  • 收稿日期:2013-06-20 修回日期:2013-08-09 出版日期:2013-10-17 发布日期:2013-10-31
  • 基金资助:

    国家自然科学基金项目(41172128);国家油气重大专项项目(2011ZX05006 - 001)

Distribution of Kaolinite and Its Influencing Factors in the Reservoir of Shahejie Formation in Dongying Depression

GUO Jia1,2,ZENG Jian-hui1,2,SONG Guo-qi3,ZHANG Yong-wang1,2,WANG Xue-jun4,MEND Wei1,2   

  1. State Key Laboratory of Petroleum Resources and Prospecting ,China University of Petroleum,Beijing 102249
  • Received:2013-06-20 Revised:2013-08-09 Online:2013-10-17 Published:2013-10-31

摘要:

高岭石广泛分布于东营凹陷沙河街组的砂岩中,对储层物性具有重要影响,但其分布特征及其控制因素目前研究得比较少。利用铸体薄片鉴定、X衍射分析、阴极发光、扫描电镜等多种测试手段研究了东营凹陷沙河街组自生高岭石的发育和分布特征及其影响因素。研究结果表明:东营凹陷沙河街组的高岭石主要在1 200~3 600 m的深度范围内分布,其中沙二段和沙三段的高岭石相对含量较高;从沙一段至沙三段,中央隆起带高岭石的平均含量均高于北部陡坡带和南部缓坡带。沙河街组砂岩储层高岭石的分布明显受有机质热演化的影响。不同的温度(埋藏深度)控制着粘土矿物的形成和转化,从而影响着沙河街组不同层段高岭石的含量及其在平面和剖面的分布。超压对高岭石的分布具有重要的影响,由于超压作用,导致超压顶界面高岭石大量发育。中央隆起带构造活动比较强,有利于酸性流体从深部向浅部充注,并且流体动力比较强,导致沙一段至沙三段中央隆起带的高岭石含量较高。断层和不整合面复合输导体系可使大量酸性流体进人浅部储层,促使浅部砂岩储层高岭石大量发育。岩性和沉积微相通过改变高岭石形成和分布的流体化学和流体动力条件,从而对高岭石分布具有重要的影响。

关键词: 高岭石, 分布特征, 影响因素, 沙河街组, 东营凹陷

Abstract:

Kaolinite widely distributed in the sandstone reservoir of the Shahejie Formation in Dongying depression,which is an important factor affecting the reservoir physical properties. But the research on its distribution characteristics and controlling factors is less comparatively. This paper goes on to research the distribution characteristics and controlling factors of kaolinite by analyzing the data from casting lamella,X-ray diffraction,cathode luminescence image,electron scan microscope. Research results show that kaolinite mainly developed in the range of depth 1,200一3,600 m. The average relatively content of kaolinite are much higher in Es2 and Es 3 .As to the kaolinite content in Es1 to Es3,the central uplift belt is higher than northern steep slope and southern ramp zone of Dongying depression. Distribution of kaolinite in the sandstone reservoirs of Shahejie Fororation is obviously affected by thermal evolution of organic matter. Different temperatures(buried depth)affect the content of kaolinite in different horizons of Shahejie Formation and its distribution in plane and profile by controlling the formation and transformation of clav minerals .The overpressure has an important influence or the distribution of kaolinite. Due to overpressure,the overpressured top boundary is generally characterized by well-developed kaolinite. Tectonic activity of central uplift belt of Dongying is strong,which is advantageous to the acidic fluid from deep to shallow filling. And hydrodynamic force is strong,leading to kaolinite content in Es1 to Es3 of the central uplift belt is higher. The pathway system composed of fault and unconformitv surface transport a large number of acidic fluid into the shallow reservoirs,which lead to considerable development of kaolinite. Lithology and sedimentary microfacies change the fluid chemistry and hydrodynamic conditions,thus has an important influence on kaolinite distribution.

Key words: kaolinite, distribution characteristic, influencing factor, Dongying depression, Shahejie Formation

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