The Shengliqiao pluton in the western Kunlun Mountains is a composite batholith.
论证了西昆仑地区的胜利桥岩体是一个复式岩基。
The late Cenozoic geomorphologic and sedimentary features in the west Kunlun Mountain front record the uplift process of the west Kunlun Mountains and the western margin of the Qinghai-Tibet Plateau.
西昆仑山前晚新生代地貌与沉积特征记录了西昆仑山及青藏高原西北缘的隆升过程。
Further study suggests that the western of the west Kunlun Mountains in the Mid-late Pleistocene has undergone at least 3 times strong upheaval.
进一步研究表明，西昆仑山地区西段中晚更新世至少经历了3次强烈的隆升。
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