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在新疆且末县黄羊沟地区首次发现蛇绿混杂岩带。该岩带由超基性岩、基性岩及石炭系、二叠系变质岩混杂堆积而成,从北向南可进一步划分为3个亚带。
The ophiolitic mélange zone was first discovered in Huangyanggou area, Qiemo County, Xinjiang. The rock zone is a mixture of ultramafic rocks, basic rocks and Carboniferous and Permian metamorphic rocks that can be further divided into 3 sub-zones from north to south.