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是泥晶-微晶白云（含膏云）的形成机。

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

为亮晶鲕粒灰和泥晶鲕粒灰，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.

准同云石化或卤水回流渗透云石化是泥-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.

原岩石为亮石灰岩和泥石灰岩，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.

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）机制。

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

原岩石为粒石灰岩和泥粒石灰岩，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.

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。