Laser Ablation (U-Th-Sm)/He Dating of Zircons: Analytical Age Bias and its Consequence for Studying Detrital Zircon Populations

IF 2.7 2区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Julien Léger, Raphaël Pik, Bouchaïb Tibari, Sébastien Ternois, Mary Ford, Chantal Peiffert, Julien Mercadier
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Abstract

The in situ (U-Th-Sm)/He and U/Pb laser-ablation double-dating procedure is a valuable method that can provide a large dataset relatively efficiently in contrast with conventional bulk helium thermochronometry. In this study, we evaluate the potential age error associated with the double ablation procedure and report the in situ (U-Th-Sm)/He double-ablation dating of 249 zircons from the Fish Canyon Tuff locality. With LA-ICP-MS pseudo-depth profiling and 3D numerical modelling, we show that the concentric double-ablation procedure in minerals with U-Th-Sm zoning can generate a significant (U-Th-Sm)/He age error (positive or negative), resulting in over-scattering and/or an offset of the mean age. Pseudo-depth profiling is insufficient to predict the individual age error, partly because of the superimposed ablations. To evaluate the consequence of this inherent bias, we confront a synthetic age distribution to the error expected for U-Th-Sm zoned zircons analysed with double-ablation (U-Th-Sm)/He thermochronometry. As expected, a strong age bias causes the spreading of peak ages, downgrading the original signal. Yet, the throughput of the ablation-based method can allow intra- and inter-sample peak age identification and comparison, and the coupling of (U-Th-Sm)/He and U/Pb ages extends our ability to deconvolute a multimodal age spectrum.

Abstract Image

锆石的激光烧蚀(U-Th-Sm)/He定年:研究碎屑锆石群体的分析年龄偏差及其后果
原位(U-Th-Sm)/He和U/Pb激光消融双测年程序是一种有价值的方法,与传统的体氦热计时法相比,它可以相对有效地提供大的数据集。在本研究中,我们评估了与双重消融程序相关的潜在年龄误差,并报告了Fish Canyon Tuff地区249个锆石的原位(U-Th-Sm)/He双重消融测年。通过LA-ICP-MS伪深度剖面和3D数值建模,我们表明,在具有U-Th-Sm分区的矿物中,同心双烧蚀过程会产生显著的(U-Th-Sm)/He年龄误差(正或负),导致过度散射和/或平均年龄偏移。伪深度剖面不足以预测个体年龄误差,部分原因是叠加消融。为了评估这种固有偏差的后果,我们采用双烧蚀(U-Th-Sm)/He热计时法分析U-Th-Sm-分区锆石,对预期误差进行了合成年龄分布。正如预期的那样,强烈的年龄偏差会导致峰值年龄的扩展,从而降低原始信号的等级。然而,基于消融的方法的吞吐量可以允许样本内和样本间峰值年龄的识别和比较,并且(U-Th-Sm)/He和U/Pb年龄的耦合扩展了我们去卷积多峰年龄谱的能力。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Geostandards and Geoanalytical Research
Geostandards and Geoanalytical Research 地学-地球科学综合
CiteScore
7.10
自引率
18.40%
发文量
54
审稿时长
>12 weeks
期刊介绍: Geostandards & Geoanalytical Research is an international journal dedicated to advancing the science of reference materials, analytical techniques and data quality relevant to the chemical analysis of geological and environmental samples. Papers are accepted for publication following peer review.
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