钻石中的密集化Mg-酸盐:对H2O运输到地幔中的影响
Luísa D V Carvalho1, Thomas Stachel1, Robert W Luth1
1University of Alberta, Department of Earth and Atmospheric Sciences, 1-26 ESB, T6G 2E3 Edmonton, AB, Canada.
Science advances
|March 13, 2024
概括
在巴西的钻石中发现了含有水的矿物质,如氧化和氧化,在巴西的钻石中发现了含水的矿物质. 这提供了地幔中脱落的状原石的直接证据.
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:
- 水显著影响上层地幔的特性,如强度和融化.
- 含有固体测量水的矿群中的矿物质是潜在的,但不太了解的挥发性储存库.
研究的目的:
- 为了识别和描述地幔衍生钻石中的含水性矿物质含量.
- 研究这些水性相对地幔过程的起源和影响.
主要方法:
- 微观观察和矿物质识别包含在一个来自巴西的钻石内.
- 矿物成分和相关矿物组合的分析.
主要成果:
- 作为地幔钻石中含有的基石和基化的观测.
- 这些含水矿物质与橄,化,含Mg的酸盐,多洛,石英,,以及djerfisherite组矿物质一起被发现.
- 相关的奥利维因显示出非地幔状的氧同位素组成,暗示了一种蛇形石原石.
结论:
- 直接证据显示,在亚地地幔的基石中,存在了废弃的围岩原石.
- 限制了地幔中水性相的稳定性.
- 洞察钻石形成流体的起源.
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