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锂同位素及其地质应用研究进展

赵葵东, 蒋少涌   

  1. 南京大学地球科学系及内生金属成矿作用国家重点实验室,江苏 南京 210093
  • 收稿日期:2001-12-20 修回日期:2001-12-20 出版日期:2001-12-20 发布日期:2001-12-20

Recent Advances in Research on Lithium Isotopes and Its Geological Applications

ZHAO Kui-Dong, JIANG Shao-Yong   

  1. State Key Laboratory for Mineral Deposits Research and Department of Earth Science, Nanjing University, Nanjing 210093, China
  • Received:2001-12-20 Revised:2001-12-20 Online:2001-12-20 Published:2001-12-20

摘要: 锂同位素示踪是近几年发展起来的一门新兴的稳定同位素地球化学方法,锂有两个稳定同位素:^6Li和^7Li。自在界锂同位素的组成变化很大,其δ^6Li值变化幅度超过60‰,现代大洋水的δ^6Li值为-31.0‰,洋中脊玄武岩(BORB)的δ^6Li值为-4.7‰--3.7‰,由于锂同位素存在大的分馏和不同地质体中在截然不同的δ^6Li值,因此锂同位素地质应用前景十分广泛。目前,锂同位素在研究星云形成过程和宇宙事件,洋壳蚀变和海底热液活动,壳-幔物质循环和板块俯冲作用过程,判断卤水起源和演化等方面的研究中成效显著。

Abstract: Lithium has two stable isotopes(6Li and 7Li)with nature abundance of 7.52% and 92.48%, respectively. Due to the large mass difference between the two lithium isotopes and low Li contents in geological samples, Li isotope measurements have met large difficulty in the past several decades. High precision Li isotope analytical methods are only developed recently, and three major methods are currently used: (1)TIMS method with analytical precision of