Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.
准同生化或卤水回流
透
化是泥晶-微晶
岩(含膏
岩)的形成机制。
Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.
准同生化或卤水回流
透
化是泥晶-微晶
岩(含膏
岩)的形成机制。
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.
组成汉盆地潜
凹陷潜
组盐间段非砂岩储层的岩
主要为泥晶
岩、钙芒硝岩、泥岩及其混积岩,孔
遍较差。
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