在古塞夫火山口由Spirit Rover分析的玄武岩石.
H Y McSween1, R E Arvidson, J F Bell
1Department of Earth and Planetary Sciences, University of Tennessee, Knoxville, TN 37996-1410, USA. mcsween@utk.edu
概括
灵魂探测器在火星的古塞夫火山口着陆地点发现了图形基岩岩. 这些岩石含有丰富的橄素和素,扩大了我们对火星地组成的理解.
科学领域:
- 地质地质地质地质地质地
- 行星科学 行星科学
- 矿物学是什么?矿物学是什么?
背景情况:
- "灵魂"探测器探索了火星上的古塞夫坑.
- 登陆地点的特点是黑暗的,细粒度的,状岩石被解释为岩.
研究的目的:
- 描述Spirit着陆地点岩石的组成和起源.
- 扩大已知的火星地组成范围.
主要方法:
- 分析Pancam和迷你热发射光谱仪 (Mini-TES) 的光谱.
- 检查经过刷磨和磨损的岩石表面的放大图像.
- 使用阿尔法粒子X射线光谱仪 (APXS) 进行化学分析.
- 莫斯巴乌尔光谱法. 莫斯巴乌尔光谱法.
主要成果:
- 岩石是相似的,但具有可变的涂层和尘埃地幔.
- 在岩石表面上可以看到变化的皮肤和静脉.
- 岩石内部含有高达25%的大晶体.
- 化学和光谱分析表明,皮克里特基岩含有规范性橄素,火素,青酸盐和FeTi氧化物.
- 确认有橄,磁石和可能的火山素.
结论:
- 分析的岩石与皮克里特基岩相一致.
- 这些发现扩大了对火星上的岩石多样性的理解.
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