石油与天然气地质 ›› 1998, Vol. 19 ›› Issue (2): 157-161,168.doi: 10.11743/ogg19980214

• 论文 • 上一篇    下一篇

赵石窑河道砂体储集特征

张运东1, 李祯2, 温显端2   

  1. 1. 中国石油天然气总公司信息研究所, 北京100011;
    2. 中国地质大学, 北京100083
  • 收稿日期:1997-08-27 出版日期:1998-06-25 发布日期:2012-01-18
  • 基金项目:

    中国石油天然气总公司“八五”重点攻关项目(85-103-01-02)

RESERVOIRING PROPERTY OF RIVER CHANNEL SANDBODIES IN ZHAOSHIYAO AREA

Zhang Yundong1, Li Zhen2, Wen Xianduan2   

  1. 1. Petroleum Information Institute, CNPC, Beijing;
    2. China University of Geosciences, Beijing
  • Received:1997-08-27 Online:1998-06-25 Published:2012-01-18

PDF (PC)

594

摘要：

赵石窑河道砂体成分成熟度和结构成熟度均较低,岩屑和长石含量较高,泥质、硅质、铁质和碳酸盐为主要填隙物,经历了同生、埋藏和表生3个成岩阶段。粒度是造成储层岩性相孔渗性差异的主要原因,可识别出8种孔隙类型和大孔-中喉、大孔-细喉、中孔-细喉和微孔-微隙型Ⅳ种孔隙结构,孔隙结构及分布与粒度和填隙物密切相关。曲流点坝相中下部孔渗性最好,底部次之,顶部及边缘最差。

关键词: 曲流河, 砂体, 微观研究, 孔喉结构, 孔隙类型, 储层物性

Abstract:

The river channel sandbodies in Zhaoshiyao area are characterized by low compositional maturation and low textural maturation,high debris and feldspar contents.The filling materials of the sandbodies are mainly argillaceous,siliceous,iron substance and carbonatite.The sandbodies underwent three diagenetic periods such as syngenetic,burial and epidiagenetic periods.Their porosity and permeability are closely related to their granularity.The porosity of the sandbodies could be classfied into 8 pore types and 4 kind of pore textures.The pore textures are related to the granularity and the filling materials.It has been proved by study that the mid and lower parts of the meandering river point bars usually have the best porosity and permeability,the bottom part is secondary and the top and marginal parts ane the worst.