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.
古岩溶发育受多种因素影响，其中古地貌形态是控制古岩溶发育及分布的主要因素之一。
Ancient karst development is affected by multiple factors, the ancient landscape is one of the major factors to control development and distribution of the ancient karst.
受潜水面阶段性上浮，相对高的古地貌上发育多期次岩溶洞穴系统。
Phased by diving surface rise, relatively high paleogeomorphology developed karst cave system in many times.
因此研究古岩溶分布规律，应先进行古地貌恢复。
The study of ancient karst distribution laws should be carried out to restore the ancient landscape.
东部地区不论在沉积微相和成岩条件，还是在古岩溶地貌上都处于不利位置，开发潜力小。
In eastern region, in terms of sedimentary microfacies and diagenetic conditions, or in karst topography are in disadvantageous position, potential for development is small.
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.
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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