Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.

准同生白云石水回流渗透白云石是泥晶-微晶白云（含膏云）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储层的石主要为泥晶白云、钙芒硝、泥及其混,渗性普遍较差。

Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.

准同生白云石化或卤水回流渗透白云石化是泥晶-微晶白云（含膏云）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石主要为泥晶白云、钙芒硝、泥及其混积,孔渗性普遍较差。

Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.

准同生白云石化或卤水回流渗透白云石化是泥晶-微晶白云岩（含膏云岩）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石主要为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.

准同生白云石化或卤水回流渗透白云石化是泥-白云岩（含膏云岩）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石主要为泥白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.

准同生白云石化或卤水回流渗透白云石化是泥晶-微晶白云岩（含膏云岩）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.

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

Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.

准同生白云石化或卤水回流渗透白云石化是泥晶-微晶白云岩（含膏云岩）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石主要为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.

准同生白云石化或卤水回流渗透白云石化是泥晶-微晶白云岩（含膏云岩）的形。

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.

组汉盆地潜凹陷潜组盐间岩储层的岩石主要为泥晶白云岩、钙芒硝岩、泥岩及其混积岩,孔渗性普遍较差。

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。

Penecontemporaneous or seepage-reflux dolomitization is the original mechanism for gypsum-bearing muddy dolomicrite.

准同石化或卤水回流渗透石化是泥晶-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石主要为泥晶岩、钙芒硝岩、泥岩及其混积岩,孔渗较差。