在Opportunity的Mossbauer光谱仪中的Meridiani Planum的石和血石
G Klingelhöfer1, R V Morris, B Bernhardt
1Institut für Anorganische und Analytische Chemie, Johannes Gutenberg-Universität, Staudinger Weg 9, D-55128 Mainz, Germany. phil.christensen@asu.edu
概括
莫斯巴乌尔光谱显示了jarosite,表明火星上过去的水性过程. 这一发现为Meridiani Planum的古代水活动提供了关键的矿物学证据.
科学领域:
- 行星科学 行星科学
- 矿物学是什么?矿物学是什么?
- 天体生物学 天体生物学
背景情况:
- 火星上的Meridiani Planum是研究过去可居住性的一个关键区域.
- 了解火星土壤和岩石的矿物学对于解释地质历史至关重要.
研究的目的:
- 用机遇探测器的数据在Meridiani Planum中识别矿物成分.
- 为了研究矿物发现对火星过去的水性过程的影响.
主要方法:
- 用机遇探测器获得的Mossbauer光谱的分析.
- 矿物学成分的识别,包括jarosite,血,olivine和pyroxene.
主要成果:
- 确定了四种不同的矿物学组成部分:亚洛和血丰富的浮岩,血丰富的土壤,含有奥利文的玄武岩土和含有烟素的玄武岩 (弹出岩石).
- 富含血的球体,被解释为混凝土,在土壤和浮岩中普遍存在.
- 证实了氧化硫酸盐矿物质jarosite的存在.
结论:
- 杰罗石的发现为火星上过去的水性过程提供了直接的矿物学证据.
- 这些水性过程可能发生在Meridiani Planum的酸硫酸条件下.
- 多样化的矿物学表明,研究区域的复杂地质和环境历史.
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