相关实验视频
Updated: Jul 25, 2026

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Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
钻石的起源,地震结构,以及卡普瓦尔-津巴布韦克拉顿的演变
Steven B Shirey1, Jeffrey W Harris, Stephen H Richardson
1Department of Terrestrial Magnetism, Carnegie Institution of Washington, 5241 Broad Branch Road NW, Washington, DC 20015, USA. shirey@dtm.ciw.edu
概括
在Kaapvaal-Zimbabwe克拉顿的地震P波速度变化.
科学领域:
- 地质物理学 地质物理学
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
背景情况:
- 卡普瓦尔 - 津巴布韦克拉顿的石层地幔包含了地球早期历史的线索.
- 了解地幔的组成对于破译克拉顿进化和钻石形成至关重要.
研究的目的:
- 为了研究卡普瓦尔-津巴布韦克拉顿的石层地幔和钻石组成中的地震P波速度之间的关系.
- 重建塑造了克拉顿及其钻石种群的石质遗传过程和地质事件.
主要方法:
- 在钻石稳定场内的各种深度对地震P波速度数据的分析.
- 地震数据与钻石的组成及其同源性含有物的相关性.
主要成果:
- 地震速度的变化与不同的钻石类型 (哈兹堡石,生态石,石英石) 和它们的包含相关.
- 中古时代的地幔枯竭事件导致了哈兹堡石钻石的形成.
- 晚期阿纪时代的增量事件引入了生态石钻石.
- 原生态时期的事件增加了更多的石和生态石钻石.
结论:
- 卡普瓦尔-津巴布韦克拉顿的石质层地幔具有复杂的枯竭,积累和变化的历史.
- 钻石成分作为一个强大的地幔过程和地质时间的cratonic进化标记器.
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