卡拉麦里断裂带是新疆北部乃至中亚地区一条显著的大型断裂带，是在古生代洋盆关闭以后形成的。
The Karamaili faulting belt is well-known in the Northern Xinjiang and Central Asian area, and it came into being after the closure of the Paleozoic ocean.
卡拉麦里断裂带是新疆北部乃至中亚地区一条显著的大型断裂带，是在古生代洋盆关闭以后形成的。
The Karamaili faulting belt is well-known in the Northern Xinjiang and Central Asian area, and it came into being after the closure of the Paleozoic ocean.
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