Application of MELTS to kinetic evaporation models of FeO-bearing silicate melts

被引：23

作者：

Alexander, CMOD ^{[1
]}

机构：

[1] Carnegie Inst Washington, Dept Terr Magnetism, Washington, DC 20015 USA

来源：

METEORITICS & PLANETARY SCIENCE | 2002年 / 37卷 / 02期

关键词：

D O I：

10.1111/j.1945-5100.2002.tb01107.x

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

Incorporation of the MELTS silicate melt solution model into models of evaporation successfully reproduces the evaporation behavior of alkali-free, FeO-bearing (greater than or equal to2 mol%) chondritic melts at temperatures between 1700 and 2000 degreesC. In conjunction with the Berman CMAS melt solution model for FeO-poor melts, evaporation of alkali-free melts can now be modeled over a very wide range of conditions. MELTS-based evaporation models can also quite successfully reproduce the evaporation behavior of K when Al/(Na+K)>1. However, reproduction of Na evaporation experiments is much poorer.

引用

页码：245 / 256

页数：12

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