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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