在机遇漫游车着陆地点的老坑和Meridiani Planum土壤
L A Soderblom1, R C Anderson, R E Arvidson
1U.S. Geological Survey, Flagstaff, AZ 86001, USA. lsoderblom@usgs.gov
概括
火星 火星 火星 火星 火星
科学领域:
- 地质地质地质地质地质地
- 行星科学 行星科学
- 沉积物学的沉积物学
背景情况:
- 机遇探测器研究了梅里迪亚尼平原 (Meridiani Planum) 的土壤.
- 这些土壤由细粒度的玄武岩砂,灰尘和富含硫酸盐的碎片组成.
研究的目的:
- 描述机遇号站点火星土壤的组成和起源.
- 了解塑造Meridiani Planum的地质过程. 为了了解塑造Meridiani Planum的地质过程.
主要方法:
- 机遇探测器对土壤和岩石样本进行分析.
- 显微镜成像和元素组成分析.
主要成果:
- 黑马球体集中在表面,通过盐化而被挖掘出来.
- 土壤被盐覆盖,可能来自地下水泥凝固.
- 由富含血的颗粒装甲的埃奥里亚波纹非常普遍.
- 土壤层厚度大约为一米.
结论:
- 土壤特征和地形表明,Meridiani Planum可能是一个古老的沉积物表面.
- 盐和风气过程在表面修饰中发挥着重要作用.
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