长江6号探测器从月球的远端采集的样本中含有28亿年历史的玄武岩
Zexian Cui1, Qing Yang1, Yan-Qiang Zhang1
1State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou, China.
概括
长江的
科学领域:
- 月球地质和地化学
- 同位素地质化学
- 星球科学
背景情况:
- 月球背面的地质与近面不同,岩石成分不同.
- ,稀土元素和 (KREEP) 在远端较少.
- 南极-艾特肯 (SPA) 盆地是研究月球背面进化的关键区域.
研究的目的:
- 在月球南极-艾特肯盆地的火山活动使用6的样本.
- 为了确定火山岩的地化学起源.
- 改进月球坑的时间模型.
主要方法:
- 月球玄武岩的与同位素分析.
- ,和同位素的分析.
- 将年龄数据整合到月球火山口时间表中.
主要成果:
- 在SPA盆地的火山活动确切年龄为2830 (±5) 百万年.
- 异位素标记表明岩来源已经耗尽了不兼容的元素.
- 岩源中含有很少或没有KREEP成分.
结论:
- 在大约28亿年前, SPA盆地经历了火山活动.
- 火山源是一个独特的月球地幔水库,与KREEP丰富的地区不同.
- 这一发现为了解月球地幔异质性和演变提供了关键数据.
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