概括
在岩石中-36的积累提供了一个新的地质计. 这种方法测量了火山岩石和地形的表面暴露时间,约会特征从1000年到100万年.
科学领域:
- 地质化学 地质化学
- 宇宙原核的约会时间
- 地质时间学 (Geochronology)
背景情况:
- 宇宙射线与矿物质的相互作用产生宇宙原核酸.
- -36 (36Cl) 在地球表面的岩石中积聚.
- 稳定化物 (Cl−) 是岩石中常见的一种元素.
研究的目的:
- 为了评估36Cl与稳定的Cl的比率,用地质计.
- 确定使用36Cl来测年年轻火山岩和地形特征的可行性.
主要方法:
- 在已知年龄的火山岩中测量36Cl度.
- 根据岩石组成和宇宙射线流量计算预测的36Cl产量.
- 分析36Cl与稳定的Cl的比率.
主要成果:
- 在被测量在日期的火山岩中的36Cl与计算的产量之间发现了良好的一致性.
- 36Cl/Cl的比率显示了作为可靠的地球时计的潜力.
- 该方法适用于表面暴露时间.
结论:
- 36Cl/Cl的比率是一个可行的地质时计,用于表面暴露的年代.
- 这种方法可以确定年轻火山岩和地形特征的年代.
- 有效的约会范围是103年至106年.
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