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.
而其余构段因也和这种大构背景分不开,只不过它们可能不单是由地东西向断裂,鄂尔多斯地中北东向基底断裂也应该起到重要作用。
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.
而其余构段因也和这种大构背景分不开,只不过它们可能不单是由地东西向断裂,鄂尔多斯地中北东向基底断裂也应该起到重要作用。
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