The Limiting Contents of Fluorine and Water in Highly Differentiated Granite Melts
- Autores: Alferyeva Y.O.1, Shchekina T.I.1, Gramenitskii E.N.1
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Afiliações:
- Department of Geology
- Edição: Volume 73, Nº 4 (2018)
- Páginas: 390-396
- Seção: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174785
- DOI: https://doi.org/10.3103/S0145875218040026
- ID: 174785
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Resumo
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.
Sobre autores
Ya. Alferyeva
Department of Geology
Autor responsável pela correspondência
Email: YanaAlf@ya.ru
Rússia, Moscow, 119991
T. Shchekina
Department of Geology
Email: YanaAlf@ya.ru
Rússia, Moscow, 119991
E. Gramenitskii
Department of Geology
Email: YanaAlf@ya.ru
Rússia, Moscow, 119991
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