The sedimentary environment of carbonate is platform facies.
碳酸盐的沉积环境主要为台地相。
The writer introduces the models of organic reef facies of platform margins and platform facies of barrier sea.
提出了台地边缘生物礁相—局限海台地相模式。
Sedimentary facies have experienced the evolutionary stages from the basin facies through platform facies to evaporite facies.
沉积相经历了从盆地相、台地相到蒸发岩相的演化过程。
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