ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
用OSL方法确定雅鲁藏布江大拐弯第四纪晚期冰川堰塞湖年龄
  
关键词:Yarlung Zangbo River  dammed lake  glacier  Quaternary  OSL
基金项目:中国地质调查局地质矿产调查评价专项(编号: 1212011120185)
作者单位E-mail
祝嵩 中国地质科学院矿产资源研究所 zhuson@gmail.com 
吴珍汉 中国地质科学院  
赵希涛 中国科学院地质与地球物理研究所  
王成敏 中国地质科学院水文地质环境地质研究所  
肖克炎 中国地质科学院矿产资源研究所  
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摘要:
The Age of Glacial Dammed Lakes in the Yarlung Zangbo River Grand Bend during Late Quaternary by OSL
      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 14C 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.
ZHU Song,WU Zhen-han,ZHAO Xi-tao,WANG Cheng-min,XIAO Ke-yan.2013.The Age of Glacial Dammed Lakes in the Yarlung Zangbo River Grand Bend during Late Quaternary by OSL[J].Acta Geoscientica Sinica,34(2):246-250.
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