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


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

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

补充文件

附件文件
动作
1. JATS XML

版权所有 © Allerton Press, Inc., 2018