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

准同白云石或卤水回流渗透白云石是泥晶-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，白云石使其岩石结构大多遭受破坏。