恢复了本区海西早期的岩溶古地貌。
And karst topography of this region in early Hercynian is recovered.
鄂尔多斯盆地南部加里东期风化壳储集层的分布主要受岩溶古地貌、风化壳层位及沉积相控制。
The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology, strata of residuum and sedimentary facies.
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.
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