昆仑山脉

和田位于新疆维吾尔自治区的西南部，塔克拉玛干沙漠与昆仑山脉之间，是历史悠久的古代绿洲之一。

As one of ancient oasis with a long history and located in the southwest of Xinjiang Uyghur Autonomous Region , Khotan stands between Taklimakan Desert and Kunlun Mountains .

途中，你可以欣赏到别样的风景：美丽的青海湖、壮观的昆仑山脉、神秘的扬子江源头、广袤的羌塘草原以及羊八井风景区。

On the way , you can view different landscapes : the beautiful Qinghai Lake , the grand Kunlun Mountains , the mysterious source of the Yangtze River , the vast Qiangtang grasslands , and the Yangpachen landscape .

这种反常现象也许可以解释为：喀拉昆仑山脉地处高纬度地区，那里的降雪量在增加，气温也更冷，冰川受全球变暖的影响较小。

This anomaly may result from increases in snowfall in the higher latitude and therefore colder karakorams , where snow and ice are less vulnerable to small temperature increases .

克里雅河发源于昆仑山脉，位置在新疆的南部。

Keriya River is located in south Xinjiang , China .

中国西部的昆仑山脉的一座山峰，海拔为英尺。

A mountain in the Kunlun range in China ( 25,340 feet high ) .

还有昆仑山脉和喀喇昆仑山脉、帕米承山脉和喜马拉雅山脉——这里把埃非尔士峰叫做珠穆朗玛峰。

The Kunlun and the Karakoram , the Pamir and the Himalayas-here Mount Everest is iknown as Chomolungma .

在昆仑山脉与雅鲁藏布缝合带之间，向东的流动便形成上部地壳的滑脱构造。

Between the Kunlun fault and Yarlung Zangbo suture the eastward flow resulted in the formation of detachments in the upper crust .

昆仑山脉和喀喇昆仑山脉地区的地壳上地幔电性结构特征

The characteristics of the electrical structure of the crust and upper mantle in the region of the Kunlun and the Karakorum Mountains

青海高原位于昆仑山脉以北，是重力高和重力低毗连出现的盆山结构。

To the north of the Kunlun fault is the Qinghai Plateau , which is a basin and range area with contiguous gravity highs and gravity lows .

新生代以来，印度板块与欧亚大陆的持续碰撞作用造就了西昆仑山脉，在西昆仑山前形成一系列的逆冲褶皱变形和大型逆冲、走滑构造。

The continuous collision of Indian plate and Euro-Asia plate since Cenozoic era formed the West Kunlun Mountains . This process also resulted in a series of deformation and large-scale strike-slip and thrust faults along the mountain front .