相关实验视频
Updated: Jul 11, 2026

08:14
Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
概括
大型岩腔可能比以前认为的更深,可能在90公里处形成. 这一发现挑战了现有的岩形成和在夏威夷海底上升的模型.
科学领域:
- 地质学和地质物理学
- 岩石学和火山学研究.
背景情况:
- 据认为,大型陆地地形岩岩 (>1000公里3) 在莫霍 (约. 在大陆下面35公里的深度).
- 这种理解限制了岩上升和分化过程的模型.
研究的目的:
- 为了研究大型岩岩的形成深度.
- 重新评估地球地幔中岩积聚和分离的过程.
主要方法:
- 来自夏威夷岛的一个不寻常的地幔石的分析.
- 石版检查识别了,橄和间石榴石.
主要成果:
- 石头的矿物质组合表明,它是在大约90公里深处的大型岩腔内形成的.
- 这种深度靠近奥阿胡岛下方古老的石化层的底部.
- 夏威夷盾牌形成的岩石可能会在喷发之前在这些深度形成池并分化.
结论:
- 大规模的岩岩可以在比以前假设的更深的深度形成.
- 深层岩室影响夏威夷岩的组成和上升.
- 复兴阶段的性 magma 和它们的 xenolith 很可能起源于石化层下方.
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