在Endeavour火山口的古代水性环境,火星
R E Arvidson1, S W Squyres, J F Bell
1Department of Earth and Planetary Sciences, Washington University in Saint Louis, St. Louis, MO 63130, USA.
概括
机遇探测器在恩德华火山口发现了过去水岩相互作用的证据,揭示了潜在的宜居环境. 岩石显示略酸到中性的pH条件有利于早期生命.
科学领域:
- 行星科学 行星科学
- 天体生物学 天体生物学
- 地质地质地质地质地质地
背景情况:
- 恩德华火山口边缘含有诺亚时代的岩石.
- 轨道光谱标志表明存在富含铁 (Fe (((+3)) 的石灰矿.
研究的目的:
- 研究恩德沃尔火山口边缘的地质历史和岩石的水性变化.
- 评估过去水性环境的可居住性.
主要方法:
- 轨道光谱反射率分析.
- 岩石断裂的实地组成分析.
- 地质绘图和地平面分析.
主要成果:
- 识别了细粒度,层层的岩石,有球体,覆盖着石.
- 检测到硫酸静脉,表明撞击后的流体循环.
- 有证据表明,富含Al的斯麦克提特通过破裂中的水性浸出而形成.
- 推断过去的水岩相互作用在轻微酸性到环中性pH环境中.
结论:
- 恩德沃尔火山口边缘保留了水岩相互作用的证据,无论是在重大撞击事件之前还是之后.
- 这些古老的水性环境可能更有利于前生物化学和微生物生命,而不是较年轻,富含硫酸盐的地点.
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