概括
斯芬U-Pb约会为古代岩石提供了可靠的年龄,通常比石产生更一致的结果. 这种方法可以确定变态事件的日期,而不仅仅是原始结晶.
科学领域:
- 地质时间学 (Geochronology)
- 同位素地球化学 同位素地球化学
- 矿物学是什么?矿物学是什么?
背景情况:
- 对古代岩石进行准确的约会对于理解地球历史至关重要.
- 斯芬 (titanite) 是各种岩石类型中常见的辅助矿物质.
- - (U-Pb) 约会是一种广泛使用的地质年代学技术.
研究的目的:
- 为了评估U-Pb约会使用sphene的可靠性.
- 为了比较体U-Pb与和生物等共存矿物质的年龄的一致性.
- 为了评估sphene在约会变形事件中的实用性.
主要方法:
- 对14个样进行了- (U-Pb) 同位素分析.
- 使用Pb-206/U-238和Pb-207/Pb-206的比率来确定年龄.
- 斯芬石的年龄与同一岩石样本中共存的石和生物石的年龄进行了比较.
主要成果:
- 斯芬样本产生了一致或几乎一致的U-Pb年龄,最大不一致率为10%.
- 在七次比较分析中,斯芬烯的年龄一致性始终高于与合存在的.
- 在两种变态岩石中,基基约定了变态的时间,而不是原始结晶.
结论:
- 斯芬是U-Pb地质年代学的可靠矿物质,特别是在古老的岩石中.
- 斯芬在许多地质环境中与石相比,提供了优越的年龄一致性.
- 斯芬U-Pb约会对于确定变形事件的时间有效.
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