摘要
采用仪器中子活化分析法测定了海南岛玻璃陨石中20多个元素的含量.通过对稀土元素及其它微量元素地球化学特征的研究,推测海南岛玻璃陨石的源岩可能是较年轻的沉积物。为了检验方法的准确度和精密度,分析了美国国家地质局的标准物质USGS—BCR—1及中国标准岩石GSRI、GSR3,其相对标准偏差小于5%。
The concentrations of more than 20 elements in the glassy meteorites from Hainan Island, China have been measured by INAA. Precision and accuracy of the INAA method have been evaluated by using USGS and Chinese standard reference materials (GSR), indicating that relative standard deviations for most element are less than 5%. A comparative study on the REE patterns and other trace elements shows that the geochemical characteristics of the glassy meteorites from Hainan Island are close to those of the Chinese continental sediment and the North America shale, implying that their parent rock is younger sediment.
出处
《核技术》
CAS
CSCD
北大核心
1996年第3期137-142,共6页
Nuclear Techniques
基金
国家自然科学基金
关键词
中子活化分析
玻璃陨石
沉积物
地球化学
Instrumental neutron activation analysis, Glassy meteorite, Sediment,Parent rock