海洋岛基岩中的Ru和W同位素系统学揭示了核心泄漏
Nils Messling1, Matthias Willbold2, Leander Kallas2
1Department for Geochemistry and Isotope Geology, Georg-August-Universität Göttingen, Göttingen, Germany. nilsmessling@gmail.com.
Nature
|May 21, 2025
概括
在夏威夷玄武岩中发现的鲁同位素异常表明核物质已经到达地球表面. 这提供了核心-地幔相互作用的证据,
科学领域:
- 地质化学
- 同位素地化学
- 星球科学
背景情况:
- 据说地幔羽毛可以从地球的核心运输物质.
- 以前的解释依赖于间接证据, 缺乏明确的核心指纹.
- 像 (Ru) 这样的贵金属集中在核心和地幔中.
研究的目的:
- 在海洋岛屿基岩中调查 (Ru) 同位素异常.
- 使用Ru同位素作为核心-地幔相互作用的新型标记物.
- 确认或反驳地幔中的核心材料的存在.
主要方法:
- 在夏威夷基岩中分析 (Ru) 同位素变化 (ε100Ru).
- 测量非放射性 (W) 同位素的比率.
- 同位素特征与环境地幔和核心组成的比较.
主要成果:
- 夏威夷的玄武岩比周围的地幔有更高的ε100Ru.
- 结合的Ru和W同位素数据显示了岩来源的核心贡献.
- 同位素系统与核心引入或核心衍生的氧化物添加一致.
结论:
- (Ru) 同位素作为一个新的,强大的核相互作用的标志物.
- 海岩提供了令人信服的证据, 核心材料通过地幔羽毛到达表面.
- 这些发现支持直接或间接将核心材料转移到地幔中的模型.
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