火星地中的橄和火氧多样性
J F Mustard1, F Poulet, A Gendrin
1Geological Sciences, Brown University, Providence, RI 02912, USA. john_mustard@brown.edu
概括
火星快递号航天器的数据显示,火星上有不同的地质矿物. 含量低,富含氧化的区域仅在古老的火星单元中发现,这表明地幔来源枯竭.
科学领域:
- 行星科学 行星科学
- 矿物学是什么?矿物学是什么?
- 地质地质地质地质地质地
背景情况:
- 火星表面的组成对于理解它的地质演变至关重要.
- 像橄,低氧化物 (LCP) 和高氧化物 (HCP) 这样的马菲克矿物质是火山活动和地幔组成的关键指标.
研究的目的:
- 在火星表面识别和绘制不同地形矿物的分布图.
- 调查这些矿产沉积物的地质背景和潜在地幔来源.
主要方法:
- 利用了来自火星快速号航天器上的矿物学,水,冰,活动观测仪器 (OMEGA) 的数据.
- 分析了光谱特征,以识别火星表面的橄,LCP和HCP.
主要成果:
- 在各种地质单位中确定了富含橄,LCP和HCP的不同区域.
- 富含奥利文和HCP的地区存在于不同年龄的沉积物中.
- 富含LCP的地区仅在古老的诺亚时代的单位中发现.
结论:
- 由于LCP的发生受到限制,这表明融的物质来源于火星上和耗尽的地幔.
- 北方平原的黑暗区域没有显著的地质或水合矿物吸收,这意味着不同的地质过程或组成.
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