鄂尔多斯盆地中央古隆起的发现。揭示了盆地古生代的构造格局。
Discovery of Central Paleouplift in Ordos basin brought light to the tectonic framework of basin in Paleozoic.
伊盟隆起地抽侧斜坡及中央古隆起四周斜坡地带，是寻找古生界天然气的有利场所；
The south slope of the northern Yimeng Uplift and the slope region around the central uplift are favorable for seeking Paleozoic natural gas.
以奥陶系顶面所刻画的中央古隆起显示：中央古隆起仅在晚寒武世-石盒子期末有所显示。
The Central Paleouplift described by Ordovician top surface was merely present during late Cambrian to last stage of Shihezi.
鄂尔多斯盆地中部气田位于稳定克拉通中央古隆起东部，是与奥陶系海相碳酸盐岩有关的风化壳型气田。
The gas field in the center of Ordos Basin is formed in the eastern central paleo-uplift of the stable craton.
鄂尔多斯盆地中部气田位于稳定克拉通中央古隆起东部，是与奥陶系海相碳酸盐岩有关的风化壳型气田。
The gas field in the center of Ordos Basin is formed in the eastern central paleo-uplift of the stable craton.
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