板内部玄武岩中的重同位素揭示了地幔中的回收碳酸盐
Rong Xu1, Yue Cai2, Sarah Lambart3
1State Key Laboratory of Critical Mineral Research and Exploration, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China.
Science advances
|April 23, 2025
概括
沉降碳酸盐,而不是蛇形岩,携带重进入地球深层地幔. 这种回收解释了板内岩石和碳酸盐中的高-11同位素特征,影响了地幔挥发性循环.
科学领域:
- 地质化学 地质化学
- 地质地质地质地质地质地
- 地球科学 地球科学 地球科学
背景情况:
- 挥发性物质回收到地幔中对于地球的可居住性至关重要.
- 较弱的脱氧化可能会阻碍深层地幔的碳运输.
- 同位素可以追踪回收的挥发物,但与地幔异质性的联系很少.
研究的目的:
- 研究同位素与地幔异质性指标的相关性.
- 确定-11 (δ11B) 成分高的来源在基岩板内.
- 评估深层地幔挥发性物质回收过程中沉降组件的作用.
主要方法:
- 在原始的大陆内板玄武岩中分析同位素.
- 检查了同位素和地幔异质性指标之间的相关性.
- 解释的同位素数据在缩地部件的背景下.
主要成果:
- 玄武岩中的同位素与地幔异质性指标相关.
- 一个共享的高δ11B组件表明回收的降温碳酸盐.
- 证据驳斥了蛇石作为这种成分的主要来源.
结论:
- 沉降碳酸盐有效地将重运送到深层地幔.
- 碳酸盐的回收利用解释了在板内岩石中观察到的高δB.
- 这一过程对深层地幔碳和挥发性循环非常重要.
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