尾闾湖

新疆主要尾闾湖演变的构造环境

Geotectonic environment of the Tail-End-Lakes evolution , xinjiang , China

在清朝，尾闾湖主要出现在现沙漠南缘。

In the Qing Dynasty , ending lakes mainly appeared in the south desert .

内陆湖泊是气候变化敏感的指示器，高山湖泊处于自然状态，受人类活动影响较小，能够较真实地反映气候状况，而内陆河尾闾湖变化是自然和人类活动共同作用的结果。

Inland lakes are sensitive indicators of climate change . High mountain lakes , due to less influence from human activity , can reflect the climate state accurately .

亚洲中部大地构造格局及地貌轮廓均以山盆体系为特征，所有封闭性盆地中都发育有尾闾湖。

The outline of geotectonic and geomorphology of the Central Asia is characterized by range and basin complex . All the closed basins develop tail-end-lake ( or lakes ) .

博斯腾湖是塔里木河流域4大源流-开都河的尾闾湖，孔雀河的源地。

The Bosten Lake is the rump lake of the Kaidu River ( one of the4 main source streams of the Tarim River ) and the source of the Kongque River .

该地在唐朝以前已经有沙漠发育，在唐朝中期元朝，这里有发源于东天山河流的尾闾湖存在，唐朝元朝将近400～500年间，可能是气候相对比较湿润的阶段。

Before the Tang Dynasty , desert has emerged in this area , since middle Tang to Yuan Dynasty , the area has ending lakes originated from East Tianshan Mountains , during the 400 ~ 500 years of Tang to Yuan Dynasty , the climate there probably is humidity relatively .