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Atom Probe Tomography Analysis of Exsolved Mineral Phases
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从地幔提供高速连接的食石喷发
Philipp Ruprecht1, Terry Plank
1Lamont-Doherty Earth Observatory of Columbia University, 61 Route 9W, Palisades, New York 10964, USA. ruprecht@ldeo.columbia.edu
Nature
|August 2, 2013
概括
由地幔衍生的岩石可以在几个月到几年的时间内穿过厚厚的地,在火山爆发期间为火山充电. 这项研究使用橄晶分析揭示了岩的快速上升,这表明对火山动荡的更深入监测.
科学领域:
- 地质化学 地质化学
- 火山学 火山学是一门学科.
- 石化学 石化学是一门学科.
背景情况:
- 汇聚边缘火山起源于地幔产生的岩石.
- 像冷却和岩混合这样的地过程掩盖了地幔爆发的联系.
- 地质物理方法在成像下层和中层地岩的动态方面存在局限性.
研究的目的:
- 为了确定地幔衍生的岩通过地上升的时间尺度.
- 为了了解地的岩腔是如何快速充电的.
- 调查地幔源与地表火山活动之间的联系.
主要方法:
- 在原始橄树中利用区分配置文件的扩散建模.
- 分析了火山爆发中初级融化的橄晶体.
- 将这种方法应用于哥斯达黎加伊拉苏火山.
主要成果:
- 地幔充电可以发生在与喷发持续时间相比的时间尺度上.
- 伊拉苏火山的岩石在几个月到几年内通过35公里的地上升.
- 层火山中的浅岩可以保留深层地幔起源的记录.
结论:
- 这项研究表明,在收边缘设置中,岩从地幔到表面的 magma 快速过渡.
- 奥利文扩散建模提供了一种新的方法来追踪岩上升时间表.
- 未来的火山动荡监测应该包括从地底部跟踪岩运动.
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