火星南极层层沉积物的积累和侵蚀
Roberto Seu1, Roger J Phillips, Giovanni Alberti
1Dipartimento INFOCOM, Università di Roma "La Sapienza," I-00184 Rome, Italy. roberto.seu@uniroma1.it
概括
详细的雷达绘制火星的地图.
科学领域:
- 行星科学 行星科学
- 地质地质地质地质地质地
- 气候科学 气候科学
背景情况:
- 火星的极地地区具有富含冰的多层沉积物.
- 这些沉积物可能保存了火星气候变化的记录.
研究的目的:
- 在火星的Promethei Lingula地区绘制详细的地表层结构图.
- 调查这些极地沉积物的结构和潜在的侵蚀历史.
主要方法:
- 在火星侦察轨道器上使用了SHARAD探测雷达仪器.
- 相关的雷达反射被解释为横跨相邻轨道轨道的层.
主要成果:
- 已识别出长达150公里的连续层.
- 观察到的离散反射序列延伸至1公里的深度.
- 在Australe Sulci中检测到浸泡层和挖掘的层,表明侵蚀.
结论:
- 澳大利亚平原的地下层结构揭示了复杂的沉积和侵蚀过程.
- 证据表明,沉积事件之间存在侵蚀时期,一些地区最近发生侵蚀.
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