在地球深处形成含量钻石的可行机制
Siyu Liu1, Wencheng Lu1, Xiaoran Zhang2
1Key Laboratory of Material Simulation Methods and Software of Ministry of Education, College of Physics, Jilin University, Changchun 130012, China; State Key Laboratory of Superhard Materials, College of Physics, Jilin University, Changchun 130012, China.
Science bulletin
|June 23, 2023
概括
科学家们发现了一种新方法,可以进入深地钻石. 这项研究解释了碳酸盐和化物在高压和高温下如何反应,在下层地幔中形成含的钻石.
科学领域:
- 地质化学 地质化学
- 矿物物理 矿物物理
- 钻石创世纪 钻石创世纪 钻石创世纪
背景情况:
- 在地球地幔中特别稀缺.
- 在亚岩层钻石中的存在对其来源和结合机制构成了重大难题.
研究的目的:
- 为了阐明含钻石的形成途径.
- 为了确定融入深地钻石的来源和机制.
主要方法:
- 化学反应的计算建模.
- 在高压和高温度 (22.5 GPa, 2100 K) 的实验验证.
- 碳酸盐 (CaCO3) 和化物 (FeB) 之间的氧化还原反应的分析.
主要成果:
- 发现了一种用于含钻石结晶的新途径.
- 在下层地幔条件下模拟和验证了CaCO3和FeB之间的氧化还原反应.
- 通过这些反应在22.5 GPa和2100 K的温度下,证明了含的钻石的形成.
结论:
- 这项研究提出了一种可行的机制,可以将融入地球地幔深处的钻石中.
- 这项研究解决了地幔中耗尽的挑战,并解释了丰富的钻石形成.
- 这些发现为下层地幔和钻石石质的地化学提供了关键的见解.
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