Email this article The Limiting Contents of Fluorine and Water in Highly Differentiated Granite Melts
- Authors: Alferyeva Y.O.1, Shchekina T.I.1, Gramenitskii E.N.1
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Affiliations:
- Department of Geology
- Issue: Vol 73, No 4 (2018)
- Pages: 390-396
- Section: Article
- URL: https://journal-vniispk.ru/0145-8752/article/view/174785
- DOI: https://doi.org/10.3103/S0145875218040026
- ID: 174785
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Abstract
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.
About the authors
Ya. O. Alferyeva
Department of Geology
Author for correspondence.
Email: YanaAlf@ya.ru
Russian Federation, Moscow, 119991
T. I. Shchekina
Department of Geology
Email: YanaAlf@ya.ru
Russian Federation, Moscow, 119991
E. N. Gramenitskii
Department of Geology
Email: YanaAlf@ya.ru
Russian Federation, Moscow, 119991
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