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月球南极-艾特肯盆地年龄为43.3亿年的证据
1Department of Earth and Environmental Sciences, The University of Manchester, Manchester, UK.
概括
月球上的南极-艾特肯盆地形成于大约43.3亿年前. 这一发现表明早期的,广泛的冲击轰炸,挑战了后期的重型轰炸理论.
科学领域:
- 行星科学 行星科学
- 月球地质学 月球地质学
- 冲击石坑的形成
背景情况:
- 南极-艾特肯 (SPA) 盆地是月球上最大和最古老的撞击结构.
- 了解SPA盆地的形成年龄对于破译太阳系内部撞击历史至关重要.
- 目前对SPA流域的年龄限制是不准确的.
研究的目的:
- 为了确定月球南极-艾特肯盆地的形成年龄.
- 改进对早期月球撞击轰炸时代的理解.
主要方法:
- 分析月球石西北非洲2995.5的化学组成.
- 流星中的矿物和岩石成分的放射测年.
- 将石石质量与SPA盆地地质学的比较.
主要成果:
- 西北非洲2995的化学成分与SPA盆地南部地区的石质学相一致.
- 放射测年法给出了大约4.324.33亿年的一致的年龄.
- 这种年龄表明SPA盆地形成在月球主要盆地集群之前约有1200万年.
结论:
- 南极-艾特肯盆地形成于大约43.3亿年前.
- 这种早期的冲击挑战了狭窄的"晚期重型轰炸"时期的概念.
- 以前的冲击盆地可能已经被SPA冲击或随后的地质过程所抹去.
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