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.
成
汉盆地潜
凹陷潜

间段非砂岩储层的岩石主要为泥晶白云岩、钙芒硝岩、泥岩及
混积岩,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.
成
汉盆地潜
凹陷潜

间段非砂岩储层的岩石主要为泥晶白云岩、钙芒硝岩、泥岩及
混积岩,孔渗性普遍较差。
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