The Limiting Contents of Fluorine and Water in Highly Differentiated Granite Melts
- Авторлар: Alferyeva Y.O.1, Shchekina T.I.1, Gramenitskii E.N.1
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Мекемелер:
- Department of Geology
- Шығарылым: Том 73, № 4 (2018)
- Беттер: 390-396
- Бөлім: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174785
- DOI: https://doi.org/10.3103/S0145875218040026
- ID: 174785
Дәйексөз келтіру
Аннотация
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.
Авторлар туралы
Ya. Alferyeva
Department of Geology
Хат алмасуға жауапты Автор.
Email: YanaAlf@ya.ru
Ресей, Moscow, 119991
T. Shchekina
Department of Geology
Email: YanaAlf@ya.ru
Ресей, Moscow, 119991
E. Gramenitskii
Department of Geology
Email: YanaAlf@ya.ru
Ресей, Moscow, 119991
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