在下层地幔中Fe-Mg分区的多变量依赖性
1Geophysical Laboratory and Center for High Pressure Research, Carnegie Institution of Washington, 5251 Broad Branch Road, NW, Washington, DC 20015-1305 USA.
地球下层地幔中铁和的分离是压力和温度依赖的. 铁铁影响矿的组成,影响深层地球的特性.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 地震学 地震学
背景情况:
- 下层地幔的组成对于理解地球的深层内部至关重要.
- 关键矿物之间的铁-分区影响地质物理性质.
研究的目的:
- 为了研究压力,温度和铁化学对下层地幔矿物分区的影响.
- 了解铁酸铁含量如何影响矿物质的稳定性和组成.
主要方法:
- 使用钻石天细胞进行高压实验.
- 在 (Fe,Mg) SiO3-矿和矿之间的铁-分区的分析.
主要成果:
- 矿稳定场随着压力和温度的增加而扩大.
- 铁性铁在矿中优先溶解,增加了表面的总铁.
- 矿中有色铁的含量随着深度而变化,在顶部耗尽并随着深度增加.
结论:
- 铁-分区是复杂的,对热力学条件和铁氧化状态敏感.
- 铁组成的变化会影响下层地幔的地球化学和地球物理特征.
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