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Surface Mapping of Earth-like Exoplanets using Single Point Light Curves
Published on: May 10, 2020
在MESSENGER首次飞越时看到的水星石坑记录.
Robert G Strom1, Clark R Chapman, William J Merline
1Lunar and Planetary Laboratory, University of Arizona, Tucson, AZ 85721, USA. rstrom@lpl.arizona.edu
概括
水星 水星 水星 水星 水星
科学领域:
- 行星科学 行星科学
- 地质地质地质地质地质地
- 冲击石坑的形成
背景情况:
- 探测器任务MESSENGER提供了关于水星表面的新数据.
- 要了解水星的地质历史,需要分析撞击坑的形成.
研究的目的:
- 通过撞击坑形态和大小频率分布来阐明水星的地质历史.
- 为了确定水星上的平原单位的年龄和起源.
主要方法:
- 从MESSENGER飞行数据分析撞击坑形态和尺寸频率分布.
- 用月球和火星数据比较火山口密度和尺寸分布.
主要成果:
- 卡洛里斯盆地的内陆平原具有相似的年龄.
- 外部光滑平原是火山产生的,而不是撞击喷射物,在38亿年前后形成.
- 在水星上,二次石坑在直径≤810公里的初级石坑上占主导地位.
- 峰环盆地Raditladi可能年龄小于10亿年.
结论:
- 水星的平原提供了对它的火山和撞击历史的见解.
- 水星上的二次石坑的普遍存在表明,与月球和火星相比,水星的撞击模式不同.
- 拉迪特拉迪盆地的年龄表明正在进行的地质活动.
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