Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.
江汉盆地潜江凹陷潜江盐间段非砂
储层的石主要为泥晶白云、钙芒硝、泥及其混积,孔渗性普遍较差。
Nonsandstone reservoirs between salt beds of Qianjiang Formation in the Qianjiang Sag of the Jianghan Basin are mainly composed of dolomicrite,glauberite rock,mudstone and their peperite.
江汉盆地潜江凹陷潜江盐间段非砂储层的石主要为泥晶白云、钙芒硝、泥及其混积,孔渗性普遍较差。
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