地球地幔中的β和ggr (Mg,Fe) 2SiO4之间的相位过渡:机制和风学影响
概括
这项研究揭示了高压下酸相变的对比机制. 这些变化影响着地球的变化.
科学领域:
- 矿物物理 矿物物理
- 地质化学 地质化学
- 固体地球地质物理学 地质物理学
背景情况:
- 酸 (Mg2SiO4) 存在于多种多态形态中,包括螺旋 () 和改性螺旋 (β).
- 了解相位转换对于解释地震数据和地幔动态至关重要.
研究的目的:
- 实验性地研究Mg2SiO4.4中马转变为β和β转变为马的机制.
- 阐明晶体结构和滑动系统在控制转化途径中的作用.
主要方法:
- 高压和高温实验在15-20 GPa和800-950°C之间进行.
- 分析相变机制,包括剪切,核和生长过程.
主要成果:
- 马转换为β转换通过剪切机制进行.
- 贝塔转变为马转变涉及谷物边界核和接口控制的生长.
- 这些不同的机制归因于每个多态的可用的独立滑动系统.
结论:
- 这两种对比的转变机制对地球地幔的浮力学和地震特性有影响.
- 预计马转变为β转变会导致潜伏区和地幔羽毛中的强度暂时减少.
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