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

准同白云石化或卤水透白云石化是泥晶-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.

准同白云化或流渗透白云化是泥晶-微晶白云（含膏云）的形成机制。

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

原为亮晶鲕粒灰和泥晶鲕粒灰，白云化作用使结构大多遭受破坏。

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（含膏云）成机制。

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

原石为亮石灰和泥石灰，白云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.

准同白云化或卤水回流渗透白云化是泥-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.

原岩为亮灰岩和泥灰岩，白云化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.

准同白云化或卤水回流渗透白云化-微白云（含膏云）的形成机制。

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

原为亮鲕粒和鲕粒，白云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.

准同白云化或流渗透白云化是泥晶-微晶白云（含膏云）的形成机制。

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

原为亮晶鲕粒灰和泥晶鲕粒灰，白云化作用使结构大多遭受破坏。

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

准同云石或卤水回流渗透云石晶-微晶云（含膏云）的形成机制。

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

原石为亮晶鲕粒石和晶鲕粒石，云石作用使其石结构大多遭受破坏。