玛曲断裂位于东昆仑断裂带的最东段。
Maqu fault is the easternmost segment of the east Kunlun active fault.
结果表明：增温异常条带在东昆仑断裂带不同段落上具有迁移特征。
The results shows:The thermally increasing anomaly belts were migrated in different segments of the east Kunlunshan fault.
该年龄与东昆中断裂附近的清水泉蛇绿岩的时代可以很好地对应起来，这为清水泉蛇绿岩带向西的延伸方向及东昆仑地区东段早古生代的构造演化提供了新的年代学证据。
This result thus provides new chronological evidence for the western extension of the Qingshuiquan ophiolite zone and the evolution of the eastern part of the east Kunlun region in Early Paleozoic.
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