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.
而其余构造段的成因也和这种大的构造背景分不开的,只不过它不单是由横穿的东西向断裂造成的,鄂尔多斯北东向的基底断裂也应该起到重要的作用。
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.
而其余构造段的成因也和这种大的构造背景分不开的,只不过它不单是由横穿的东西向断裂造成的,鄂尔多斯北东向的基底断裂也应该起到重要的作用。
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