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西藏西部冈仁波齐花岗闪长岩锆石SHRIMP U-Pb定年及其地质意义
引用本文:夏斌,韦振权,张玉泉,徐力峰,李建峰,王彦斌. 西藏西部冈仁波齐花岗闪长岩锆石SHRIMP U-Pb定年及其地质意义[J]. 地质通报, 2007, 26(8): 1014-1017
作者姓名:夏斌  韦振权  张玉泉  徐力峰  李建峰  王彦斌
作者单位:1. 中国科学院广州地球化学研究所边缘海地质重点实验室,广东,广州,510640
2. 中国科学院广州地球化学研究所边缘海地质重点实验室,广东,广州,510640;中国科学院研究生院,北京,100039
3. 北京离子探针中心,北京,100037
摘    要:冈底斯岩带西段冈仁波齐岩体斑状花岗闪长岩中的锆石SHRIMPU-Pb年龄测定结果为48.3Ma±1.5Ma,该年龄反映了冈仁波齐花岗闪长岩体的侵位或结晶年龄,属于喜马拉雅期,相当于中始新世。岩体的形成时间略晚于印度-欧亚大陆初始碰撞的时间,为两大陆碰撞作用过程中的产物,属同碰撞花岗岩。

关 键 词:锆石SHRIMP U-Pb定年  花岗闪长岩  冈仁波齐  冈底斯岩带西段  西藏
文章编号:1671-2552(2007)08-1014-04
修稿时间:2007-01-10

SHRIMP U-Pb zircon dating of granodiorite in the Kangrinboqê pluton in western Tibet, China and its geological implications
XIA Bin,WEI Zhen-quan,ZHANG Yu-quan,XU Li-feng,LI Jian-feng,WANG Yan-bin . Key Laboratory of Marginal Sea Geology,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou,Guangdong,Chin,. Graduate School of the Chinese Academy of Sciences,Beijing,Chin,. Beijing SHRIMP Center,Beijing,China. SHRIMP U-Pb zircon dating of granodiorite in the Kangrinboqê pluton in western Tibet, China and its geological implications[J]. Geologcal Bulletin of China, 2007, 26(8): 1014-1017
Authors:XIA Bin  WEI Zhen-quan  ZHANG Yu-quan  XU Li-feng  LI Jian-feng  WANG Yan-bin . Key Laboratory of Marginal Sea Geology  Guangzhou Institute of Geochemistry  Chinese Academy of Sciences  Guangzhou  Guangdong  Chin  . Graduate School of the Chinese Academy of Sciences  Beijing  Chin  . Beijing SHRIMP Center  Beijing  China
Affiliation:XIA Bin,WEI Zhen-quan,ZHANG Yu-quan,XU Li-feng,LI Jian-feng,WANG Yan-bin . Key Laboratory of Marginal Sea Geology,Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou,Guangdong,Chin,. Graduate School of the Chinese Academy of Sciences,Beijing,Chin,. Beijing SHRIMP Center,Beijing,China
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