在地幔化过程中,金组元素的分解
Conny Bockrath1, Chris Ballhaus, Astrid Holzheid
1Institut für Mineralogie, Universität Münster, Corrensstrasse 24, 48149 Münster, Germany. bockrat@nwz.uni-muenster.de
概括
在星球上层地幔中存在两个稳定的硫化物相:单硫化物和硫化物化物. 这些阶段分别控制了贵金属在剩余地幔和玄武构件中的分布.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 矿物物理 矿物物理
背景情况:
- 上层地幔中硫化物相的组成和行为对于理解贵金属 (白金组元素) 循环至关重要.
- 以前的研究还没有完全阐明不同硫化物相在地幔融和融分离过程中的不同作用.
研究的目的:
- 在上层地幔条件下,研究硫化物-酸盐系统中硫化物相的稳定性和分离.
- 确定这些硫化物阶段如何影响残留地幔和分离酸的贵金属含量.
主要方法:
- 使用硫化物-酸盐系统的石油实验.
- 分析相组合和贵金属分区的分析.
主要成果:
- 两个不同的硫化物相是稳定的:一个以Os,Ir和Ru丰富的晶体单硫化物,以及以Rh,Pt和Pd丰富的硫化物化物.
- 在酸盐融分离过程中,单硫化物留在固体残留物中,控制残留地幔的贵金属特征.
- 硫化物融化物以液滴形式融入化物融化物中,定义了玄武岩岩的贵金属库存.
结论:
- 单硫化物和硫化物融阶段的独特行为导致贵金属在残余地幔和岩石之间有明确的分割.
- 这种理解对于追踪地幔过程和PGEs在岩石矿石沉积中的起源至关重要.
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