概括
新的分析技术使得稀土矿物质的-176/哈夫-176测年成为可能. 这项研究完善了-176的半衰期,证实了地质和物理测量.
科学领域:
- 地质化学 地质化学
- 射线测量约会的方法
- 同位素地球化学 同位素地球化学
背景情况:
- -176/哈夫-176 (176Lu/176Hf) 同位素系统是地质测年的强大工具.
- 以前的局限性阻碍了这种方法在克尺寸的稀土元素 (REE) 丰富矿物质上应用.
研究的目的:
- 开发和应用先进的分析技术,精确测量 (Lu) 和 (Hf) 同位素.
- 为了使176Lu/176Hf地质计能够应用于含有稀土的较大矿物样本.
- 从地质上重新确定176Lu.半衰期.
主要方法:
- 开发专门的分析和同位素稀释技术,用于微克级别的Lu和Hf.
- 这些方法应用于含有REE的矿物质的克数量.
- 对176Lu半衰期的地质重新确定.
主要成果:
- 成功地将176Lu/176Hf方法应用于克尺寸的矿物样本.
- 在微克水平上精确测量Lu和Hf同位素.
- 176Lu的重新确定地质半衰期为3.3 +/- 0.5 x 10 10年.
结论:
- 开发的分析技术显著提高了176Lu/176Hf约会方法的适用性.
- 176Lu的新半衰期值与最近的物理测量结果一致,增强了地球时间学准确性.
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