The distribution of ophiolites is very wide in China. 我國蛇綠岩分佈廣泛。
Therefore, the Qingshuigou ophiolites may be the product of island-arc volcanic activity, and probably generated in the fore or back-arc tectonic settings. 所以中祁連清水溝蛇綠岩屬島弧火山活動的產物，可能形成於弧前或者弧后的構造環境。
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