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
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隶属关系:
- 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.
作者简介
Ya. Alferyeva
Department of Geology
编辑信件的主要联系方式.
Email: YanaAlf@ya.ru
俄罗斯联邦, Moscow, 119991
T. Shchekina
Department of Geology
Email: YanaAlf@ya.ru
俄罗斯联邦, Moscow, 119991
E. Gramenitskii
Department of Geology
Email: YanaAlf@ya.ru
俄罗斯联邦, Moscow, 119991
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