赵晓莉;李和平;苏根利;

• 1:中国科学院地球化学研究所地球内部物质高温高压实验室
• 2:中国科学院研究生院

摘要(Abstract)：

高温高压水流体中矿物的溶解度是研究地球内部水流体-固体相互作用过程中元素活化、迁移和沉淀以及热液组成、性状及演化的必备参数。石英作为地壳最基本的组成矿物,其在高温高压水流体中的溶解度在地球内部热液作用研究中具有极为重要的意义,迄今已有许多学者对石英在高温高压水流体中的溶解度作过研究。本文通过系统总结前人有关研究成果,从实验技术、影响因素以及石英的赋存状态和溶解度模型等方面介绍了高温高压水流体中石英溶解度的研究进展,对目前该研究存在的问题作出了评述,并对未来该研究的发展趋势进行了预测。

关键词(KeyWords)： 高温高压;水流体;石英;溶解度;研究进展

Abstract:

Keywords:

基金项目(Foundation): 国家自然科学基金项目(批准号:40373034);; 中国科学院大型设备研制项目(资助号:YZ200720)

作者(Authors): 赵晓莉;李和平;苏根利;

DOI: 10.16461/j.cnki.1000-4734.2013.01.011

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