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东昆仑造山带中发育的NW向线性构造带具有等间距特征 ,其组合以区域剪切带为主体 ,显示多层次、多期次及深切性区域深断裂的基本属性。是具隐爆特征的镁铁质岩 -闪长玢岩组合的浅成杂岩体和五龙沟、托克妥金、铜矿床的导岩、导矿通道及赋存场所。NW向线性构造带是东昆仑地区寻找五龙沟玢岩型金矿床的重要标志
The NW-trending linear tectonic belts developed in the East Kunlun orogenic belt have equidistance characteristics. The combination of these zones is mainly composed of regional shear zones and shows the basic properties of deep faults in multi-level, multi-stage and deep zones. It is characterized by epithermal magmatite-dioritic porphyrite assemblage of shallowly-compacted complex rock, guide rock of Wulonggou, Torkutudin gold and copper deposit, guide channel and site of deposit. The NW-trending linear tectonic belt is an important indicator for finding Wulonggou porphyry gold deposits in the East Kunlun area