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阿尼玛卿蛇绿混杂岩带位于东昆仑东段南缘,处于秦祁昆缝合系和古特提斯缝合系(Bian,1996)的交接部位。蛇绿岩带呈NWW向延展,长约400km,宽10—50km;由一系列构造岩片构成。在其西段的布青山-牧羊山蛇绿混杂岩带见有晚二叠-三叠纪砂板岩角度不整合在此蛇绿混杂岩之上,不整合面之
The Animaqing ophiolitic melange belt is located at the southern margin of the eastern Kunlun Mountains in the junction of Qin Qikun suture and the ancient Tethyan suture (Bian, 1996). The ophiolite zone is NWW-extended, about 400 km long and 10-50 km wide; it consists of a series of tectonic slices. The Late Permian-Triassic sand slate shows unconformity on the ophiolitic mélange in the Bujushan-Maiyu ophiolitic melange belt in the western part,