摘要
随着实验地球化学的快速发展,元素在熔/流体系中的分配行为引起研究者的广泛关注。自二十世纪70年代以来,研究者对元素在硅酸盐熔/流体系中的分配行为进行了大量研究,并取得了一些重要成果。本文对近30年来国内外在该领域的研究现状进行了归纳、总结,探讨了固相组成、金属元素本身的物理化学性质、流体组分中阴、阳离子对硅酸盐熔/流体系中元素分配行为的影响,并指出了当前研究中存在的主要问题,希望对今后的实验研究起到一定的借鉴作用。
With the development in experimental geochemistry, researchers pay more and more attention to element partition coefficient between silicate solid/liquid coexisting system People have done much work in this aspect and attained many important results since 1970This paper summarized the literature in this subject in the late 30 years, and discussed element partition behavior between the solid/liquid phases from the following aspects: the composition of the solid phase, the physical and chemical characters of the metal elements, and the cation and anion composition of the liquid phase Some important questions have been put forward in the research at present It will be useful for future research work
出处
《地质地球化学》
CSCD
2003年第3期88-92,共5页
Geology-Geochemistry
基金
国家杰出青年基金(49925309)
国家重点基础研究发展规划项目(G1999043209)
关键词
实验地球化学
元素
熔/流体相
分配系数
experimental geochemistry
element
solid/liquid phase
partition coefficient
