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《Acta Geoscientica Sinica》 2013-02
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The Age of Glacial Dammed Lakes in the Yarlung Zangbo River Grand Bend during Late Quaternary by OSL

ZHU Song 1) , WU Zhen-han 2) , ZHAO Xi-tao 3) , WANG Cheng-min 4) , XIAO Ke-yan 1) 1) Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037; 2) Chinese Academy of Geological Sciences, Beijing 100037; 3) Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029; 4) Institute of Hydrogeology and Environmental Geology, Chinese Academy of Geological Sciences, Shijiazhuang, Hebei 050061  
The Yarlung Zangbo River is a great river in the Tibetan Plateau, and the landform of river valley and geological evolution history of its development has an important significance for the study of the Tibetan Plateau geology. Previous researchers tested lacustrine sediments by ESR and 14 C methods in the Yarlung Zangbo River valley and recognized four periods of dammed lakes. The authors analyzed lacustrine samples with OSL (Opically Stimulated Luminescence) and got the ages of (50.9± 2.1) ka BP and (1.8 ±0.1) ka BP. These data suggest that the Yarlung Zangbo Great Bend had two ancient dammed lakes existent respectively during the early stage of the last glacial period and the new glacial period.
【Fund】: 中国地质调查局地质矿产调查评价专项(编号:1212011120185)资助
【CateGory Index】: P343.6
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