概括
由于一种特定的反应,钻石和碳酸盐可以在地幔生态石中共存. 这一发现解释了地质构造和含钻石岩石的保存.
科学领域:
- 地质化学 地质化学
- 矿物学是什么?矿物学是什么?
- 石化学 石化学是一门学科.
背景情况:
- 钻石和碳酸盐是地球地幔的关键组成部分.
- 了解它们的共存,可以了解地幔过程.
研究的目的:
- 在生态矿石中定义了控制钻石和碳酸盐共存的反应.
- 为了比较氧气流动性条件,以确定生态矿石与矿石中的钻石稳定性.
主要方法:
- 反应的热力学分析:多洛米特+2可西特<=>二氧化+2钻石+2O(2).
- 氧气流动性 (fO2) 条件的比较.
主要成果:
- 多洛米特+2可西特<=>二氧化+2钻石+2O(2) 反应定义了生态矿石中钻石碳酸盐的共存.
- 生态石钻石的稳定性发生在~1log单位高的氧气流动性,而不是在peridotites.
- 这种差异使得含有钻石的生态石与含有碳酸盐的岩石共存.
结论:
- 显著的氧气流动性条件解释了观测到的生态石和石的地质联系.
- 这可以解释无碳的桃石与含有钻石的石榴石火石 (摩洛哥Beni Bousera山脉).
- 它还解释了具有钻石的生态石异石的优越保存,而不是石异石 (罗伯茨·维克多·金伯石).
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