来自澳大利亚西部杰克希尔斯 (Jack Hills) 的石钻石
Martina Menneken1, Alexander A Nemchin, Thorsten Geisler
1Institut für Mineralogie, Westfälische Wilhelms-Universität, Corrensstr. 24, 48149 Münster, Germany. m_menn03@uni-muenster.de
Nature
|August 24, 2007
概括
在425亿年前的杰克希尔斯石中发现的最古老的陆地微钻石表明,早期的地球有厚厚的大陆地,并且经历了地和地的相互作用. 这一发现重新塑造了我们对早期地球演化和钻石形成的理解.
科学领域:
- 地质科学是地球科学.
- 矿物学是什么?矿物学是什么?
- 早期地球的历史 历史 历史
背景情况:
- 杰克·希尔斯石是已知的最古老的地碎片,为早期地球提供了洞察力.
- 以前的研究表明,早期大陆地的回收和花岩融生产.
研究的目的:
- 为了研究杰克希尔斯古老的圆体内的微钻石含有.
- 为了确定这些微型钻石的年龄和特性.
- 根据钻石发现,推断早期地球演化的条件.
主要方法:
- 用显微镜检查detrital石内部的入物.
- 子含有物的放射测年.
- 钻石含的拉曼光谱学.
- 矿物协会 (石墨) 的分析.
主要成果:
- 在杰克·希尔斯石中发现了微钻石入,年龄为3.058至4.252亿年.
- 这些是已知的地球岩石中最古老的钻石.
- 钻石矿物学类似于超高压转化过程中形成的钻石.
结论:
- 这些发现暗示相对厚厚的大陆石化层至少存在于425亿年前.
- 这表明在海底或 Eoarchean 时代发生了显著的地-地幔相互作用.
- 年龄分布表明重复的钻石形成条件或古老的钻石回收.
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