The distribution of Caledonian residuum reservoirs in the south of Ordos Basin is mainly controlled by karst palaeogeomorphology, strata of residuum and sedimentary facies.
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。
2
There developed a vast area of weathering crust karst reservoirs on top Ordovician in Ordos Basin.
鄂尔多斯盆地在奥陶系顶部发育大面积的风化壳岩溶储层。
3
There are closer relations among pore groundwater system, Karst groundwater system and fissure groundwater system in Taiyuan basin.