古地貌特征决定了层间岩溶作用的发育程度。
The ancient landform characteristic has decided the growth degree of the interlayer karst process.
同生期层间岩溶；
因此古地貌高地、古地貌斜坡与洼地中的局部地貌隆起将是层间岩溶作用发育的最有利区带。
Therefore the partial landform uplift among the ancient landform highland, the ancient landform slope and the marsh land will be most advantageous area belt of the growth of interlayer karst process.
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