概括
这项研究表明,高温和高压可以导致石的损失显著,支持地质时代学中的偶发性损失模型. 这影响了-测年准确度.
科学领域:
- 地质化学 地质化学
- 同位素地质学的同位素.
- 变态石器学 变态石器学
背景情况:
- 中的- (U-Pb) 同位素系统对地质年代学至关重要.
- 了解损失机制对于准确的放射测年是至关重要的.
- 甲基石是易受变化和同位素干扰的.
研究的目的:
- 为了研究金属中-同位素系统的干扰.
- 在特定的实验条件下量化损失.
- 评估对地质年代学解释的影响.
主要方法:
- 试验改变一个metamict塞隆石.
- 在2莫拉NaCl溶液中处理,温度为500°C,流体压力为1000bar.
- 分析-同位素比率以确定损失.
主要成果:
- 实现了-同位素系统的显著干扰.
- 在13天内观察到61%的放射性损失.
- 实验条件表明,对的同位素完整性有很大的影响.
结论:
- 实验结果支持情节性损失模型,而不是连续模型.
- 这一发现对自然体U-Pb系统的解释有重大意义.
- 准确的地质年代测定需要考虑这种干扰事件.
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