在火星的恩德沃尔火山口,古代撞击和水性过程
S W Squyres1, R E Arvidson, J F Bell
1Department of Astronomy, Cornell University, Ithaca, NY 14853, USA. squyres@astro.cornell.edu
概括
火星探测器Opportunity在恩德沃尔火山口的边缘发现了丰富和石膏静脉. 这些发现表明过去的热水活动和火星地区的潜在可居住条件.
科学领域:
- 行星科学 行星科学
- 地质地质地质地质地质地
- 天体生物学 天体生物学
背景情况:
- 火星探测器"机遇"探测了恩德沃尔火山口,这是一个古老的撞击地点.
- 石坑边缘的沉积物由冲击产生的玄武岩石石组成,显示出类似地球的层状结构.
研究的目的:
- 研究恩德沃尔火山口边缘的地质特征和化学成分.
- 确定局部丰富物和静脉系统的来源.
- 评估对过去可居住性和水活动的影响.
主要方法:
- 机遇探测器对火星表面材料进行现场分析.
- 地质化学研究破碎石的组成和静脉矿物学.
- 冲击沉积物的平流图分析.
主要成果:
- 在材料中发现了局部丰富,这表明了热水变化.
- 观察到富含石膏的静脉在石坑边缘附近的沉积岩中切割.
- 证据表明,从边缘上流的低温水性流体的降水.
结论:
- 在恩德沃尔火山口发生了热水变化,其证据是丰富.
- 石膏静脉表明过去的低温水性流体流动,创造了暂时可居住的条件.
- 这些流体有助于形成Meridiani Planum富含硫酸盐的砂岩.
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