发现一个沉重的同位素地幔储存库
Mao-Rui Liu1,2, Jun Wang1, Ze-Xian Cui1
1State Key Laboratory of Deep Earth Processes and Resources, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China.
National science review
|December 1, 2025
概括
同位素 (δ30Si) 数据揭示了以前未知的地幔储库. 沉降的大陆地融化,产生高δ30Si的融化,丰富了石化地幔.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 地幔石器学地幔石器学
背景情况:
- (Si) 循环是地球过程的关键.
- 地幔衍生的岩显示出可变的同位素 (δ30Si) 组成.
- 含量高于土 (BSE) 的 δ30Si 的水库是隐含的,但未被确定.
研究的目的:
- 研究地幔岩石中的同位素变异.
- 在地幔衍生的岩石中确定异常 δ30Si 的来源.
- 了解循环,其中涉及沉积的大陆地.
主要方法:
- 分析了同位素 (δ30Si) 数据,这些数据来自代灯矿石.
- 检查了来自喜马拉雅-西藏原始物质的宿主地幔氧化物 (pyroxenite xenoliths).
- 在地幔-地相互作用的背景下解释同位素特征.
主要成果:
- 兰普罗伊特和石的 δ30Si 值高于BSE.
- 升高的δ30Si来源于矿和印度大陆地的融之间的反应.
- 粗融化产生补充的高δ30Si融和低δ30Si残留物.
结论:
- 沉降的大陆地可以产生高δ30Si的化物.
- 这些融化物将石质层的地幔转化为体,形成富含的水库.
- 和残留物不均分布会影响地幔循环.
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