摘要
大牛地气田盒2、3段的成岩作用主要包括压实作用、胶结作用、交代作用和溶蚀作用。该区主要孔隙类型以粒间和粒内溶蚀孔隙和晶间微孔为主,原生孔隙基本消失。据统计,该区储层属于低孔、低渗型储层。高岭石的晶间微孔对储层孔隙的贡献有重要作用,而方解石对储层影响包括破坏和建设两个方面。次生加大石英、绿泥石、伊利石则对储层的孔渗有明显的破坏作用。
The diagenesis of Member He2 and Member He3 in Daniudi gas filed includes compaction, cementation, dissolution and denudation. The main pore types of the reservoir in this area are dissolution pores between grains and in grains and intergranular micropore, and primary pores almost disappear. The reservoir has low permeability and low porosity. The intergranular micropores of kaolinite greatly contribute to reservoir pores, while the calcite influences the reservoir both from damage and construction. Overgrowth quartz, chlorite and Illite obviously reduce the permeability and porosity of the reservoir.
出处
《大庆石油地质与开发》
CAS
CSCD
北大核心
2007年第6期28-30,35,共4页
Petroleum Geology & Oilfield Development in Daqing
基金
国家自然科学基金项目(40672078)资助
关键词
大牛地气田
低孔低渗
成岩作用
储层
Daniudi gas field
low permeability and low porosity
diagenesis
reservoir
作者简介
吝文（1980-）男，湖北广水人，在渎博士，从事沉积储层研究工作。
