相关实验视频
Updated: Jun 28, 2026

06:14
Simulating Imaging of Large Scale Radio Arrays on the Lunar Surface
Published on: July 30, 2020
月球背面的长期火山活动由SELENE地形摄像机揭示
Junichi Haruyama1, Makiko Ohtake, Tsuneo Matsunaga
1Institute of Space and Astronautical Science, Japan Aerospace Exploration Agency, 3-1-1 Yoshino-dai, Sagamihara, Kanagawa 229-8510, Japan. haruyama.junichi@jaxa.jp
概括
月球背面的海火山活动在很大程度上在30亿年前停止了. 然而,一些沉积物显示较年轻的年龄 (约25亿年前),表明长期和可能是月球上的偶发火山活动.
科学领域:
- 月球地质学 月球地质学
- 星球科学 星球科学
- 石坑的时间计量仪.
背景情况:
- 海洋沉积物是月球火山历史的关键指标.
- 以前的研究表明,月球火山活动的停止更为均.
研究的目的:
- 为了确定月球背面的海沉积物的年龄.
- 为了完善月球海火山活动的时间表.
主要方法:
- 利用了来自SELENE的地形摄像机的10米分辨率图像.
- 分析了石坑的频率分布,以建立模型年龄.
主要成果:
- 大多数月球背面的海火山活动大约在30亿年前结束.
- 几个海沉积物表现出明显较年轻的年龄,大约25亿年前.
- 这表明马火山活动的持续时间比以前认为的要长.
结论:
- 月球背面的月球海火山活动持续时间比预期的更长.
- 火山活动可能是偶尔发生的,具有明显的年轻阶段.
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