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4.1 Ga old detrital zircon in western Tibet of China
作者姓名:DUO  Ji  WEN  ChunQi  GUO  JianCi  FAN  XiaoPing  LI  XiaoWen
作者单位:[1]Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 850000, China [2]Chengdu University of Technology, Chengdu 610059, China
基金项目:Supported by National 973 Project (Grant No.2002CB412600) and the National Natural Science Foundation of China (Grant No.40472058)
摘    要:4.1 Ga old detrital zircon was found by SHRIMP U-Pb dating for quartz schist from Buring County in western Tibet, Southwest China. This is the oldest zircon U-Pb age found in China so far. The detrital zircon is a zircon of magmatic origin because its Th/ U ratios are 0.76 to 0.86. Two dates older than 4.0 Ga were measured only in one grain. U-Pb ages of 35 measured spots in 24 zircons can be subdivided into 6 groups, corresponding to at least 6 episodes of magmatic activity in the target area. The present results provide an important geochronological constraint on the geological evolution of Qinghai-Tibet Plateau.

关 键 词:锆石  中国  西藏  地层
收稿时间:3 July 2006
修稿时间:2006-07-032006-09-25

4.1 Ga old detrital zircon in western Tibet of China
DUO Ji WEN ChunQi GUO JianCi FAN XiaoPing LI XiaoWen.4.1 Ga old detrital zircon in western Tibet of China[J].Chinese Science Bulletin,2007,52(1):23-26.
Authors:Duo  Ji  Wen  ChunQi  Guo  JianCi  Fan  XiaoPing  Li  XiaoWen
Institution:(1) Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa, 850000, China;(2) Chengdu University of Technology, Chengdu, 610059, China
Abstract:4.1 Ga old detrital zircon was found by SHRIMP U-Pb dating for quartz schist from Buring County in western Tibet, Southwest China. This is the oldest zircon U-Pb age found in China so far. The detrital zircon is a zircon of magmatic origin because its Th/ U ratios are 0.76 to 0.86. Two dates older than 4.0 Ga were measured only in one grain. U-Pb ages of 35 measured spots in 24 zircons can be subdivided into 6 groups, corresponding to at least 6 episodes of magmatic activity in the target area. The present results provide an important geochronological constraint on the geological evolution of Qinghai-Tibet Plateau.
Keywords:SHRIMP U-Pb dating  detrital zircon  4  1 Ga  China
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