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.
而其余构段的成因和这种大的构分不开的,只不过它们可能不单是由横穿盆地的东西向断裂成的,鄂尔多斯盆地中北东向的基底断裂起到重要的作用。
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.
而其余构段的成因和这种大的构分不开的,只不过它们可能不单是由横穿盆地的东西向断裂成的,鄂尔多斯盆地中北东向的基底断裂起到重要的作用。
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