在火星早期分化过程中形成的异质地幔和地结构
James M D Day1, Marine Paquet1,2, Arya Udry3
1Scripps Institution of Oceanography, University of California San Diego, La Jolla, CA 92093, USA.
Science advances
|May 31, 2024
概括
纳克莱特和查西尼特石是来自单一的火星岩源. 它们揭示了火星内部有着古老的地,一个大体化的地幔石化层,以及一个耗尽的深层地幔.
科学领域:
- 行星科学 行星科学
- 地质化学 地质化学
- 宇宙化学 宇宙化学
背景情况:
- 纳克利特和哈西尼特是火星的石,具有独特的地化学特征.
- 以前的研究已经讨论了这些石群体的起源和关系.
研究的目的:
- 为了研究纳克莱特和查西尼特石的岩起源.
- 为了阐明火星早期内部的组成和结构.
主要方法:
- 对高度 siderophile 元素丰度的分析.
- 纳克莱特和查西尼特石的奥斯 (Os) 同位素地质化学.
主要成果:
- 纳克利特和哈西尼特代表的是一个来自火星的岩套件.
- 纳赫利特石显示了同化古老的证据,改变了玄武岩地 (>20亿年前).
- 未被吸收的纳克利特和哈西尼特表明,它们是从枯竭的岩层地幔中提取的,与雪戈提特石来源不同.
结论:
- 火星拥有多层层的内部,包括古老的丰富的玄武岩地,一个大体化地幔石化层,以及一个耗尽的深层地幔.
- 这种分层结构为火星早期的岩和地质演变提供了洞察力.
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