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Meanwhile, the I-, S- and A-type granitoids in the northern Kunlun region were formed by intracontinental subduction of the central Kunlun subplate along the Mid-Kunlun fault in late Triassic epoch.
昆北区出露的I型、S型、A型花岗岩，形成于昆中板片，在晚三叠世沿昆中断裂发生的陆内俯冲。
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