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《Quaternary Sciences》 2002-05
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QUATERNARY GLACIATIONS IN THE WEST NYAIQENTANGLHA MOUNTAINS

Zhao Xitao ① Wu Zhonghai ② Zhu Dagang ② Hu Daogong ② (① Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029; ② Institute of Geomechanics, CAGS, Beijing 100081)  
Along the south and north feets as well as in individual valleys of the West Nyaiqentanglha Mountains, there are three sets of Pleistocene glacial deposits. The first set is distributed at the feet of Nyaiqentanglha, constituting the high piedmont moraine platforms 150~350 m higher than the valley bottoms. On their front margins, there are always simultaneous high fluvioglacial platforms. The second set is mainly distributed in glacial troughs cutting the mountains and their outlets, constructing the high lateral and terminal moraines 30~80m higher than the valley bottom. The third set is also distributed in glacial troughs, constituting the low lateral and terminal moraines 5~15m higher than the valley bottom. In front of the Xibu glacier extended over ten kilometers, the longest one in the West Nyaiqentanglha Mountains, there are also three groups of Holocene terminal moraines. Three glacitions corresponding to the three sets or groups of moraines are named in this paper the Ninzhong Glaciation (0.7~0.6MaB.P.), the Paran Glaciation (0.2~0.14 MaB.P.), and the Laqu Glaciation (0.07~0.03 MaB.P.). Their ages are determined by methods of ESR, U-series, and OSL. Glaciers due to the three Pleistocene glaciations are various: large-scale piedmont glaciers, middle- and small-scale valley glaciers and small-scale valley glaciers. The Xibu glacier advanced two times: one in the Neoglaciation and one in the Little Ice Age. In last decades, however, it retreated obviously. Finally, through compositional correlations of the preglacial, glacial and modern gravels with rocks in three structural strata of the Nyaiqentanglha Mountains, the denudation and uplift of the mountains were discussed and the history of glacial evolution was traced.
【Fund】: 中国地质科学院 1∶2 5万当雄幅地质调查 (批准号 :DKD990 1 0 0 1 );; “西藏纳木错第四纪环境演变调查研究”(批准号 :DKD2 0 0 1 0 0 6 )资助项目
【CateGory Index】: P343.6
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