石油与天然气地质 ›› 1992, Vol. 13 ›› Issue (2): 167-174.doi: 10.11743/ogg19920205

• 论文 • 上一篇    下一篇

吉木萨尔凹陷仓房沟群火山砂岩的典型成岩反应及其物性特征

楼章华, 赵霞飞   

  1. 成都地质学院 610059
  • 收稿日期:1989-09-06 修回日期:1990-05-16 出版日期:1992-06-25 发布日期:2012-01-16

TYPICAL DIAGENETIC REACTIONS AND PHYSICAL PROPERTY OF VOLCANIC SANDSTONE IN CHANGFANGGOU GROUP,JIMOSAL DEPRESSION

Lou Zhanghua, Zhao Xiafei   

  1. Chengdu College of Geology
  • Received:1989-09-06 Revised:1990-05-16 Online:1992-06-25 Published:2012-01-16

PDF (PC)

642

被引次数

13

摘要：

近地表碳酸盐化和浅埋藏水化水解,使火山砂岩在压实前固结,其中的粒间孔隙被以蒙脱石为主的自生粘土矿物充填或分割。决定孔隙水性质和形成自生粘土矿物及沸石等离子,来自火山砂岩本身。火山砂岩的典型成岩反应是水化水解和脱水反应,决定了孔隙水的性质、成岩矿物组合和储层的物性。

关键词: 准噶尔盆地, 火山砂岩, 水化水解作用, 脱水作用, 储层物性, 孔隙组合

Abstract:

The volcanic sandstone had been cemented by calcitization near the ground and by shallow buried hydration-hydrolysis,the intergranular pores of which were filled and separated by authigenic clay minerals.The typical diagenetic reactions of the volcanic sandstone were hydration-hydrolysis and dehydration which decided the property of pore water,the assemblage of diagenetic minerals and the physical property of the reservoir bed.