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U and Th zonation in Fish Canyon Tuff zircons: Implications for a zircon (U-Th)/He standard

机译:Fish Canyon Tuff zircons中的U和Th分区:对锆石(U-Th)/ He标准的影响

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摘要

The inability to accurately determine the distribution of U and Th in zircon crystals analysed using (U-Th)/He is a major source of error, and limits the confidence in subsequent data interpretation. The Fish Canyon Tuff (FCT) zircon standard shows (U-Th)/He age reproducibility in excess of ±10%. We have tested the extent to which this is due to U and Th zonation using a combination of cathodoluminescence and ion probe analysis of a population of FCT zircons. Primarily we find that FCT zircons exhibit extreme U and Th zonation, and the population has large inter-crystalline variability. Furthermore, the net cathodoluminescence intensity from the FCT zircons is negatively correlated with U and Th concentration, allowing cathodoluminescence emission to be used as a proxy for U and Th zonation. This correlation was exploited to constrain the U and Th zonation within the crystal population, and to show that the poor age reproducibility of the FCT zircons is consistent with the observed zonation. © 2008 Elsevier Ltd. All rights reserved.
机译:无法准确确定使用(U-Th)/ He分析的锆石晶体中U和Th的分布是主要的误差来源,并限制了后续数据解释的可信度。鱼峡谷凝灰岩(FCT)锆石标准显示(U-Th)/ He年龄再现性超过±10%。我们使用阴极荧光和结合了FCT锆石的离子探针分析,测试了这归因于U和Th分区的程度。首先,我们发现FCT锆石显示出极高的U和Th带,并且该族群具有较大的晶间变异性。此外,来自FCT锆石的净阴极发光强度与U和Th浓度呈负相关,从而使阴极发光发射可用作U和Th分区的代理。利用这种相关性将U和Th区域限制在晶体种群中,并显示FCT锆石的较差的年龄再现性与观察到的区域一致。 ©2008 Elsevier Ltd.保留所有权利。

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