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月球背面火山活动28亿年前从6基石
Qian W L Zhang1, Mu-Han Yang1,2, Qiu-Li Li3,4
1State Key Laboratory of Lithospheric and Environmental Coevolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing, China.
Nature
|November 15, 2024
概括
月球背面的火山活动持续了超过14亿年,样本显示了420亿年前的KREEP丰富来源和年轻基岩的KREEP贫乏来源. 这证实了远端石坑的年代模型.
科学领域:
- 月球地质
- 星球科学
- 地质时间学
背景情况:
- 了解月球的火山历史是解释它的半球差异的关键.
- 之前的研究表明长期存在的远端火山,但缺乏样本证据.
研究的目的:
- 使用返回的样本调查月球背面的火山历史.
- 验证和完善月球背面的石坑时间模型.
主要方法:
- 在Chang'e-6任务中返回的基岩碎片的Pb-Pb年代.
- 分析U-Pb同位素组成以确定源特性 (μ值).
主要成果:
- 确定了两个基岩火山事件:一个来自KREEP丰富来源的4,203±4万年前 (最古老的返回样本),一个来自KREEP贫乏来源的较年轻的2,807±3万年前.
- 较年轻的火山活动年龄与火山口计数估计一致,
- 证明月球背面的火山活动持续了超过14亿年.
结论:
- 月球背面的火山活动是长期存在的,从KREEP丰富的来源演变为KREEP贫乏的来源.
- 6号任务提供了远端火山历史的重要样本证据.
- 两个月球半球都适用于火山口的时间表模型.
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