摘要
溶蚀作用是四川盆地龙王庙组白云岩储层形成的关键。本文在四川盆地龙王庙组白云岩储层中识别出同生期溶蚀作用、表生期溶蚀作用、埋藏溶蚀作用,并且分别总结了他们的主要特征。通过对溶蚀作用的认识进而探讨深层碳酸盐岩储层孔隙保存机理,为下一步的勘探开发提出建议。
Dissolution is the key for the formation of dolomite reservoirs of Dragon King Temple Formation in Sichuan basin. This article to identify syngenetic dissolution, supergene period dissolution and burial dissolution in the dolomite reservoir of Dragon King Temple Formation in Sichuan basin, besides, it sums up their main characteristics respectively. Through the understanding of dissolution to discuss the pore preservation mechanism of deep-seated carbonate reservoir so that to give suggestions for further exploration and development.
作者
陈阳
陈晶晶
王克鑫
朱烨
Chen Yang Chen Jingjing Wang Kexin Zhu Ye(School of Resource and Environment of Yangtze University, Hubei,430100 Shiyan Taihe Hospital in Hubei province, Hubei,442000)
出处
《当代化工研究》
2016年第8期3-4,共2页
Modern Chemical Research
关键词
龙王庙组
同生期溶蚀作用
表生期溶蚀作用
埋藏溶蚀作用
Dragon King Temple Formation
syngenetic dissolution
supergene period dissolution
burial dissolution
