来自地球下层的蓝色含量钻石
Evan M Smith1, Steven B Shirey2, Stephen H Richardson3
1Gemological Institute of America, New York, NY, USA. evan.smith@gia.edu.
Nature
|August 3, 2018
概括
蓝色钻石揭示了深层地幔的回收. 这些罕见的宝石中的表明海洋地向下层地幔浸入,促进钻石形成和地元素回收.
科学领域:
- 地质化学
- 矿物学
- 石油学
背景情况:
- 板块构造驱动了地球地幔的表面物质循环.
- 由于释放的深度较浅,因此难以追踪地的组成部分.
- 在地中很丰富, 在地深层形成钻石的液体中发现.
研究的目的:
- 为了确定深层层钻石中的的来源.
- 为了确定IIb型钻石结晶的地质设置.
- 阐明海洋岩层在深层地幔过程中的作用.
主要方法:
- 在含的钻石中分析矿物质含量.
- 高压/高温实验以确定矿物质的稳定性.
- 潜水过程的地化学建模.
主要成果:
- 含的钻石含有独特的矿物质组合.
- 这些组合表明前体在更低地幔深度的海洋石化层中稳定.
- 证据表明,海洋石化层中的被压缩并释放到深层流体中.
结论:
- 类型IIb的钻石来自下层地幔,是已知的最深层钻石之一.
- 海水蛇形化的海洋石化层为回收进入深层地幔提供了途径.
- 这项研究证明了深层地元素的可行回收机制.
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