概括
- (Re-Os) 同位素分析揭示了石和铁石之间的差异. 地石显示出明显的Re-Os闭合年龄,这表明早期太阳星云中的形成历史各不相同.
科学领域:
- 宇宙化学 宇宙化学
- 地质时间学 (Geochronology)
- 同位素地球化学 同位素地球化学
背景情况:
- - (Re-Os) 同位素系统是确定石形成年龄的强大工具.
- 之前的研究为铁石建立了同位素,为Re-Os关闭年龄提供了参考.
研究的目的:
- 为了确定Re和Os的度和Os的同位素组成,在各种石和铁石.
- 为了比较Re-Os同位素系统学在地铁和铁石之间推断形成历史.
主要方法:
- 使用共振电离质谱法 (RIMS) 精确确定Re和Os度和同位素成分.
- 分析了八个碳状石,一个普通石 (Semarkona LL3) 和两个铁石.
主要成果:
- 铁石的Re-Os和Os同位素比率与已建立的铁石同位素时间保持一致.
- 大多数石数据图表在铁石同位素上方的1-2%以上,表明不同的Re-Os关闭年龄或前体材料.
- 特定的混凝土 (Semarkona LL3,Murray C2M) 的图形显著更高,这表明通过水性变化或原始同位素异质性可能发生Re损失.
结论:
- 石和铁石可能是从具有不同的化学历史的前体材料中形成的.
- 观察到的一些混凝土中的同位素变异可能反映了形成后的过程,如早期太阳星云中的水性液或同位素异质.
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