用户名: 密码: 验证码:
The Diagenesis and Pore Evolution of Sandstone Reservoir of Xusi Sector in Fenggu Area, West Sichuan Province
详细信息   
摘要

    

///According to the study on the thin section of well Fenggu 21 and well Chuanfeng 563 and the geology analysis, the authors think the main reservoir space of calc sandstone reservoir is the secondary solution pore and fissure owing to the solution process, which must belong to the fissure-pore type. The fluid which forms the calcite in pore and fissure is mainly resulted from the resolution carbonate rock detritus in the calcarenaceous sandstone.

© 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