用户名: 密码: 验证码:

The Evolution Mode and Controlling Factors of Pore Space Ofoolitic Shoal Reservoir in Feixianguan Formation in Northeast Sichuan Basin

详细信息   
摘要
Based on outcrops and core observation in Northeast Sichuan, granite slices and scanning electron microscopic pictures, combined with the relationship between sizes, shapes, genesis and rock structure of oolitic reservoir in Feixianguan Formation, this paper makes a study on the characteristics, evolution mode and controlling factors of various types of pore space of oolitic reservoir in Feixianguan Formation in Northeast Sichuan area. The results indicate that pore types include residual intergranular pores, intergranular dissolution porosity, intragranular porosity, intergranular holes, intergranular porosity and fractures. The evolution mode of pore space can be divided into 3 types: oolitic limestone shoal type, oolitic dolomite shoal type and non-phase-controlled type. The formation of pore space is controlled by sedimentation, diagenesis and tectogenesis.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700