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

准同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。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原岩石为亮晶鲕粒石灰岩和泥晶鲕粒石灰岩，白云石化作用使其岩石结构大多遭受破坏。

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

同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。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原岩石为亮晶鲕粒石灰岩和泥晶鲕粒石灰岩，白云石化作用使其岩石结构大多遭受破。

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

准同白云水回流渗透白云是泥晶-微晶白云岩（含膏云岩）的形成机制。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原岩为亮晶鲕粒灰岩和泥晶鲕粒灰岩，白云作用使其岩大多遭受破坏。

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

准同白云或卤水回流渗透白云是泥晶-微晶白云岩（含膏云岩）的形成机制。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原岩为亮晶鲕粒灰岩和泥晶鲕粒灰岩，白云用使其岩结构大多遭受破坏。

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。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原岩石为亮晶鲕粒石灰岩和泥晶鲕粒石灰岩，石化作用使其岩石结构大多遭受破坏。

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

准同白石化或卤水回流渗透白石化是晶-微晶白（膏）的形成机制。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原石为亮晶鲕粒石灰晶鲕粒石灰，白石化作用使其石结构大多遭受破坏。

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

准同白化或卤水回流渗透白化是泥晶-微晶白（含）的形成机制。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原为亮晶鲕和泥晶鲕，白化作用使其结构大多遭受破坏。

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

准同或卤水回流渗透是泥晶-微晶岩（含膏岩）的形成机制。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原岩为亮晶鲕粒灰岩和泥晶鲕粒灰岩，作用使其岩结构大多遭受破坏。

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

准同白云石化或卤水回流渗透白云石化是泥-微白云岩（含膏云岩）的制。

The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures.

原岩石鲕粒石灰岩和泥鲕粒石灰岩，白云石化作用使其岩石结构大多遭受破坏。