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现代地质 ›› 2007, Vol. 21 ›› Issue (4): 691-696.

• 能源地质学 • 上一篇    下一篇

甘肃酒泉盆地青西油田裂缝特征及成因分析

李军1,2,王德发1,范洪军1   

  1. 1中国地质大学  能源学院,北京100083;2中国石油 玉门油田分公司,甘肃 玉门735200
  • 收稿日期:2007-01-21 修回日期:2007-05-21 出版日期:2007-04-20 发布日期:2007-04-20
  • 作者简介:李军,男,高级工程师,博士研究生,1971年出生,石油地质学专业,主要从事油气田开发的地质研究工作。 Email:lijun_8596@yahoo.com.cn。

A Description of Fracture Features and Its  Formation Mechanisms in Qingxi Oilfield, Jiuquan Basin,Gansu

LI Jun1,2,WANG De-fa1,FAN Hong-jun1   

  1. 1School of Energy Resources, China University of Geosciences, Beijing100083,China;
    2Yumen Oilfield Company, PetroChina, Yumen, Gansu735200,China
  • Received:2007-01-21 Revised:2007-05-21 Online:2007-04-20 Published:2007-04-20

摘要:

甘肃酒泉盆地青西油田泥砾岩相和泥云岩相储层中发育两种裂缝系统。采用多种方法,系统研究了不同岩相区裂缝的产状特征、电性响应特征和物性特征,并重点分析了控制裂缝形成的成岩演化成因。研究结果表明:泥砾岩相中发育有砾缘缝、粒内溶蚀缝和构造裂缝;泥云岩相中发育层面溶蚀缝、泄水裂缝及构造裂缝。裂缝系统不但对储层渗流能力有较大程度的改善,而且也具有一定程度的储集能力。母岩矿物的选择性(差异)溶蚀是控制本区裂缝和次生孔隙发育的主要因素:泥砾岩成分复杂,各种碎屑物及胶结物之间的交代、溶蚀以及不稳定碎屑颗粒的选择性(差异)溶蚀是砾缘缝、成岩溶蚀缝及大量次生孔隙在泥砾岩储层中形成的主要原因;泥云岩中存在的二元和三元纹层结构从根本上决定了裂缝的发育程度,碳酸钙的白云岩化和沸石化是层面溶蚀缝形成的主要成岩作用。

关键词: 青西油田, 酒泉盆地, 泥砾岩, 泥云岩, 裂缝特征, 成岩作用, 选择性(差异)溶蚀

Abstract:

There are two types of fractures in the muddy gravel and the tuffaceous dolomite in Qingxi oilfield, Jiuquan Basin. By applying many kinds of techniques, the characters of fracture pattern, log response and reservoir quality in different lithofacies are systematically studied, and the diagenesis of controlling fracture is thoroughly analyzed. The results show that gravel-edge fractures, corrosion fractures and structure fractures are formed in muddy gravel rocks; lay fractures, extrusion fractures and structure fractures formed in tuffaceous dolomite. The fracture systems not only improve mainly the  permeability, but also increase the porosity. The selective(diverse)corrosion diagenesis of parent rock is the main factor, which controls the forming of fractures and secondary pores. There are several mineral components in muddy gravel and the key reason to muddy gravel fractures is the replacement of the framework grain and cement, the dissolutions of the cement and dissolvable grain. Dual and trinal structures are the key to fracture systems in the tuffaceous dolomite, which includes strong dolomitization and laumontitization in carbonitites.

Key words: Qingxi oilfield, Jiuquan Basin, muddy gravel, tuffaceous dolomite, fracture feature, diagenesis, selective(diverse)corrosion

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