摘要
川西成都盐盆某4井的中三叠系雷口坡组雷四段储层中富含富钾卤水。我们根据富钾卤水的赋存特征,结合其地质构造特点,利用有限的几条常规测井曲线,总结出该类储层的测井相应特征,并建立起岩石物理模型,确定其解释参数和岩石骨架参数,为该类储层的测井解释工作奠定了良好的基础。
Well No.4 in Chengdu Salt Basin in west Sichuan is enriched with potassium-rich brine in the reservoir of No.4 Member of Leikoupo Formation of the Middle Triassic System.According to the enrichment characteristics of potassium-rich brine in combination with its characteristics of geologic structure and by means of several limited normal logging curves, correspondent characters of logging in such reservoir is summarized and petrophysical model is established.Explanatory paramters and petro-skeleton parameters are determined, which has laid a solid foundation for well logging explanation.
出处
《中国井矿盐》
CAS
2008年第6期11-14,共4页
China Well and Rock Salt
关键词
成都盐盆
富钾卤水
测井解释
Chengdu Salt Basin,potassium-rich brine
well logging explanation
