The siliceous rock zone in Yantong mountain area, central Jilin Province, is the key region for studying the paleo-Asian ocean tectonic evolution.
吉林中部烟筒山地区的硅质岩带是研究古亚洲洋构造演化的一个关键地区。
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.
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。
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