The Limiting Contents of Fluorine and Water in Highly Differentiated Granite Melts

Ya. O. Alferyeva; T. I. Shchekina; E. N. Gramenitskii

doi:10.3103/S0145875218040026

The Limiting Contents of Fluorine and Water in Highly Differentiated Granite Melts

作者: Alferyeva Y.O.¹, Shchekina T.I.¹, Gramenitskii E.N.¹
隶属关系:
1. Department of Geology
期: 卷 73, 编号 4 (2018)
页面: 390-396
栏目: Article
URL: https://journal-vniispk.ru/0145-8752/article/view/174785
DOI: https://doi.org/10.3103/S0145875218040026
ID: 174785

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详细

The content of water was estimated in acid aluminosilicate and brine aluminofluoride melts in equilibrium. The solubility of water reaches 7–8 wt % in a silicate melt and 15–19 wt % in an aluminofluoride melt. The maximum concentration of fluorine in an aluminosilicate melt increases with increasing water content in the system.