摘要
现代和古代蒸发石盐中流体包裹体去除实验表明,利用在马弗炉中爆裂石盐流体包裹体的方法可以在很大程度上除去残存的微小流体包裹体。爆裂法较无水乙醇研磨法能更有效地消除流体包裹体的影响,从而可进一步提高固相石盐中微量元素的测试精度。
The experimental results of removal of fluid inclusions in modern and ancient evaporative halites show that the decrepitation method can remove the remained small fluid inclusions to a large degree.The decrepitation method is more effective in eliminating the influence of small fluid conclusions than the method of cracking halite in ethanol,and the measurement precise of trace elements in solid halite can improve further.
出处
《盐湖研究》
CSCD
2011年第1期16-19,共4页
Journal of Salt Lake Research
基金
国家自然科学基金项目(40903014)
中科院知识创新工程重要方向项目(KZCX2-YW-344)
关键词
石盐
爆裂法
流体包裹体
微量元素钾、镁
Halite
Decrepitation method
Fluid inclusion
Trace elements K and Mg
