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天然气地球科学 ›› 2012, Vol. 23 ›› Issue (4): 691–699.doi: 10.11764/j.issn.1672-1926.2012.04.691

• 天然气地质学 • 上一篇    下一篇

川西丰谷构造须家河组四段钙屑砂岩优质储层控制因素

林煜，吴胜和,徐樟有,倪玉强   

  1. 1.中国石油大学(北京)地球科学学院，北京 102249;
    (2.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:2012-03-20 修回日期:2012-04-23 出版日期:2012-08-10 发布日期:2012-08-10
  • 通讯作者: 林煜lin66yu@163.com. E-mail:lin66yu@163.com.
  • 作者简介:林煜（1985-），男，陕西延长人，博士研究生，主要从事精细油藏描述及开发地质研究. E-mail：lin66yu@163.com.
  • 基金资助:

    国家科技重大专项(编号：2011ZX05009-003)；国家油气重大专项（编号：2011ZX05031-003）联合资助.

Controlling Factors for T3x4 Calcarenaceous Sandstone in Fenggu Structure，Western Sichuan Basin

LIN Yu，WU Sheng-he，XU Zhang-you，NI Yu-qiang   

  1. 1.College of Geoscience,China University of Petroleum,Beijing 102249,China;
    2.State Key Laboratory of Petroleum Resource & Prospecting,China University of Petroleum,Beijing 102249,China
  • Received:2012-03-20 Revised:2012-04-23 Online:2012-08-10 Published:2012-08-10

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摘要：

钙屑砂岩在整个川西坳陷须家河组四段广泛发育，且普遍致密。采用铸体薄片、扫描电镜、物性分析和水岩实验等手段，对丰谷构造须四段钙屑砂岩的基本特征进行了分析，探讨了沉积环境、成岩作用和构造运动对该类型优质储层形成的控制作用.结果表明，研究区钙屑砂岩分选中等—好，成分成熟度低，主要的储集空间为粒间溶孔和残余粒间孔，属特低孔特低渗储层。沉积作用和成岩作用是钙屑砂岩优质储层形成的主控因素。其中，发育在高能相带、且碳酸盐岩岩屑含量高（＞90%）是钙屑砂岩优质储层发育的先决条件；而埋藏成岩过程中有机酸的溶蚀、烃类的早期充注和早期方解石胶结物的少量生成是钙屑砂岩优质储层孔隙保存及次生溶孔形成的关键。

关键词: 钙屑砂岩, 特低孔特低渗储层, 控制因素, 沉积特征, 成岩作用, 构造运动, 须四段

Abstract:

Upper Triassic Xujiahe calcarenaceous sandstone is widespread and tight in the west Sichuan depression.The high-quality reservoir of calcarenaceous sandstone was firstly touched in the Fenggu structure in 2005.It is change the view that calcarenaceous sandstone can not form reservoir.So far,the controlling factors for the formation of high quality reservoir of calcarenaceous sandstone are unclear.In this paper,we use cast thin-sections,scanning electron microscope,physical analysis,and water-rock interaction to describe the basic characteristics of T3x4 calcarenaceous sandstone in the Fenggu structure.We discuss the potential reasons including sedimentary environment，diagenesis and tectonic movement to control the formation reasons of high-quality reservoir of calcarenaceous sandstone.The results show that the calcarenaceous sandstone is characterized by medium-well sort,low compositional maturity and medium-fine grained.The reservoir space bears dissolved pores between grains and residual intergranular pores,belonging to extra-low porosity and extra-low permeability reservoir.Sedimentary and diagenesis are major factors for the formation of high-quality reservoir of calcarenaceous sandstone.Among them,the favorable sedimentary facies zone and high calcarenaceous content are the preconditions to form high-quality reservoir.The dissolution of organic acids,filling of early hydrocarbons and cementation of early carbonates under the buried process are the keys to form high-quality reservoir.

Key words: Calcarenaceous sandstone, Extra-low porosity and extra-low permeability reservoir, Controlling factor, Sedimentary character, Diagenesis, Tectonic movement, 4th member Xujiahe Formation

中图分类号: 

  • TE122.2

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