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在深层地幔条件下融玄武岩的结构变化
Chrystèle Sanloup1, James W E Drewitt, Zuzana Konôpková
11] Centre for Science at Extreme Conditions and School of Physics and Astronomy, University of Edinburgh, Scottish Universities Physics Alliance, Edinburgh EH9 3JZ, UK [2] Université Pierre et Marie Curie, UMR-CNRS 7193, Institut des Sciences de la Terre Paris, F-75005, Paris, France.
Nature
|November 9, 2013
概括
高压改变了酸融化的结构,影响了地球的深层过程. 这项研究揭示了协调在化玄武岩中如何在极端压力下发生变化,影响融化的压缩性和元素分区.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 高压科学科学 高压科学
背景情况:
- 酸盐液体对于地球的进化至关重要,从早期形成到火山活动.
- 了解在高压下酸融化的行为对于定量地球模型至关重要.
- 实验挑战在历史上对地球深层酸融化的数据有限.
研究的目的:
- 为了研究高压下融玄武岩的结构变化和压缩机制.
- 为了确定与地球地幔相关的酸盐化的状态方程.
- 探索融化压缩能力对 siderophile 元素分区的影响.
主要方法:
- 在现场使用X射线衍射来探测融玄武岩的结构.
- 实验是在高达60千兆帕斯卡尔 (GPa) 的压力下进行的.
- 分析的重点是协调和融化密度的演变.
主要成果:
- 在化玄武岩中,协调率从4增加到6增加了35 GPa.
- 在协调变化后,融的压缩能力显著下降.
- 一个高阶状态方程是必要的,以准确地模拟地幔压力下的密度.
结论:
- 在酸盐融中观察到的结构转变会影响它们的压缩性.
- 在高压下化的压缩性会影响像这样的元素在铁和酸盐之间进行分离.
- 这些发现为建模深层地球过程和核心-地幔相互作用提供了关键数据.
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