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晶白云岩、钙芒硝岩、岩及其混积岩,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晶白云岩、钙芒硝岩、岩及其混积岩,孔渗性普遍较差。
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