The cause of formation of other section is similar to 38°N zone, but they shaped not only by transmeridional fault but also by north-east orientation fundus faults of Ordos basin.
而其余构造段的和这种大的构造背景分不开的,只不过它们可能不单是由横穿盆地的东西向断裂造的,鄂尔多斯盆地中北东向的基底断裂应该起到重要的作。
The cause of formation of other section is similar to 38°N zone, but they shaped not only by transmeridional fault but also by north-east orientation fundus faults of Ordos basin.
而其余构造段的和这种大的构造背景分不开的,只不过它们可能不单是由横穿盆地的东西向断裂造的,鄂尔多斯盆地中北东向的基底断裂应该起到重要的作。
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