西部Medusae Fossae形成的hesperian年龄,火星的时间
James R Zimbelman1, Stephen P Scheidt
1Center for Earth and Planetary Studies, MRC 315, National Air and Space Museum, Smithsonian Institution, Washington, DC 20013-7012, USA. zimbelmanj@si.edu
概括
火星上的Medusae Fossae形成 (MFF) 显示了其在盖尔火山口附近扩展的新证据. 撞击坑的数量表明了对MFF历史和火星上层次材料的修订理解.
科学领域:
- 行星科学 行星科学
- 火星地质学 火星地质学
背景情况:
- 梅杜萨岩坑 (Medusae Fossae Formation,简称MFF) 是火星上一个大,被侵蚀的沉积物,位于火山口高地以北.
- 人们普遍认为,MFF是由火岩喷发形成的.
研究的目的:
- 研究Medusae Fossae形成的地质历史和范围.
- 分析MFF在盖尔火山口附近新发现的材料的影响.
主要方法:
- 西部Medusae Fossae形成的地质测绘.
- 撞击坑计算在MFF单位上.
主要成果:
- 多年框架材料的异常值被确定超出了以前绘制的边界,延伸到盖尔火山口附近.
- 撞击坑分析提供了关于MFF单位年龄的新数据.
结论:
- 这些发现扩大了Medusae Fossae形成的已知范围.
- 石坑的数量为MFF的历史和盖尔石坑的层层沉积提供了洞察力.
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