火星的盖尔火山口的矿被盐水驱动的破坏
T F Bristow1, J P Grotzinger2, E B Rampe3
1Eobiology Branch, NASA Ames Research Center, Moffett Field, CA 94035, USA. thomas.f.bristow@nasa.gov.
概括
探测器的数据显示,在古老的火星湖泊岩石中, 这一发现表明火星早期存在广泛的酸盐矿物不稳定,影响了地质和天体生物学过程.
科学领域:
- 地质学
- 天体生物学
- 星球科学
背景情况:
- 火星的沉积岩提供了关于古代地质和天体生物学过程的见解.
- 探测器正在调查盖尔火山口的夏普山, 检查35亿年前的湖床层.
研究的目的:
- 分析时间等价沉积岩中的矿物学空间变化.
- 了解盐水在古火星岩层变化的作用.
主要方法:
- 探测器从维拉鲁宾山脉穿越至格伦托里登.
- 在距离不到400米的沉积岩层中进行矿物学分析.
主要成果:
- 在相当时间的岩层中观察到矿物学的显著空间差异.
- 这些变化归因于局部透的盐.
结论:
- 与硫酸盐沉积相关的贫盐水透,局部改变的沉积岩.
- 硫酸盐沉积物的广泛分布表明,这种盐水驱动的酸盐不稳定是火星早期的常见过程.
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