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月球上有22亿年的富含KREEP的火山活动
Mu-Han Yang1, Qian W L Zhang2, Qiu-Li Li1
1State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing 100049, China.
Science bulletin
|September 3, 2025
概括
最年轻的月球石显示了长期的KREEP (,稀土元素,) 岩,延长了8亿年的时间. 这表明月球地幔过程是月球火山晚期的燃料.
科学领域:
- 月球地质
- 同位素地质化学
- 星球科学
背景情况:
- 月球的KREEP成分是火山活动的关键热源.
- 的任务数据质疑KREEP在火山活动的后期阶段的作用.
研究的目的:
- 调查与KREEP相关的月球岩的持续时间和来源.
- 分析已知最年轻的月球石以了解晚期火山活动.
主要方法:
- 月球石NWA16286的地化学和地时间分析.
- 收集和分析月球基岩的同位素数据.
主要成果:
- NWA 16286的年代为2.201±1300万年前,显示了一个富含KREEP的地幔源.
- 这延长了KREEP相关的岩石流量约8亿年.
- 月球玄武岩表现出三个火山事件,其中U/Pb同位素增加,而Nd同位素减少,表明地幔对流.
结论:
- 连续发生的地幔颠覆或羽毛驱动的上升引发了月球火山活动.
- 在较年轻的火山事件中,KREEP的成分越来越多地被纳入玄武岩源.
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