一个干燥的月球地幔储存器为年轻的基岩
Sen Hu1, Huicun He2, Jianglong Ji2
1Key Laboratory of the Earth and Planetary Physics, Chinese Academy of Sciences, Beijing, China. husen@mail.iggcas.ac.cn.
Nature
|October 19, 2021
概括
五号任务揭示了月球最年轻的火山活动并非由丰富的水驱动. 月球基岩的分析表明地幔的来源是脱水的,这表明水被早期的火山过程所移除.
科学领域:
- 月球地质
- 宇宙化学
- 星球科学
背景情况:
- 月球上的水分布影响了月球的起源和演变.
- 五号任务返回了年轻的马岩 (年龄20亿年).
研究的目的:
- 调查石中的水含量和同位素.
- 确定月球地幔中年轻火山活动的水量.
主要方法:
- 分析Chang'e-5基岩中的岩和岩融物.
- 测量水的丰度和/的比率.
主要成果:
- 在原始岩中最多含水量为283±22μg/g.
- 原始岩的/比为 (1.06 ± 0.25) × 10−4.
- 估计的地幔水的最大丰度:1-5μg/g.
结论:
- 最年轻的月球火山 (Chang'e-5) 并不是由水驱动的.
- 由于先前的融化提取,地幔源区域可能已经脱水了2.0亿年.
- 这表明月球的地幔含水量较早.
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