孔德鲁和富含和的含有物中的同位素年龄
Yuri Amelin1, Alexander N Krot, Ian D Hutcheon
1Department of Earth Sciences, Royal Ontario Museum, Toronto, ON M5S 2C6, Canada. yamelin@NRCan.gc.ca
概括
石中的富含和含 (CAI) 和体的形成发生在数百万年的时间里. 这项研究为这些早期太阳系事件提供了精确的年龄限制.
科学领域:
- 太空化学 太空化学
- 行星科学 行星科学
- 地质时间学 (Geochronology)
背景情况:
- 富含和的含有物 (CAI) 和体是石的原始组成部分.
- 了解它们的形成时间表对于揭示早期太阳系过程至关重要.
研究的目的:
- 准确地确定CV型冠状状体中CAI形成和CR型冠状体中chondrules形成之间的年龄间隔.
- 为了限制早期太阳系中CAI和chondrule形成事件的持续时间.
主要方法:
- 在Acfer 059石中,孔德鲁的-同步测年.
- 在埃弗雷莫夫卡石中CAI的同位素约会.
- 对初始26Al/27Al比率的分析.
主要成果:
- 红线的-等离子年龄为4564.7±0.6万年.
- CV CAI 的同位素年龄为 4567.2 ± 0.6 Ma.
- 这表明CV CAI和CR冠状管形成之间有2.5±1.2万年 (My) 的间隔,事件至少持续1.3万年.
结论:
- 在太阳系早期,CAI和chondrule形成跨越了相当长的时期.
- 确定的时间间隔与基于26Al-26Mg系统的时间表一致.
- 这支持了26Al-26Mg同位素比在太阳系材料约会中的时间意义.
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