Advancing (U-Th)/He Zircon Dating: Novel Approaches in Sample Preparation and Uncertainty Reduction

IF 1.8 4区 地球科学 Q3 GEOCHEMISTRY & GEOPHYSICS
Y. Hao, Ying Wang, Zhuqi Zhang, Jingxing Yu, Yizhou Wang, J. Pang, Wanfeng Zhang, Dewen Zheng
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Abstract

The laser microprobe (U-Th)/He dating method is a new and efficient technique that utilizes an interoperable and integrated suite of instruments, including the excimer laser system, quadrupole helium mass spectrometer, and quadrupole inductively coupled plasma mass spectrometer. To demonstrate the applicability of this new method, we applied both the conventional and laser microprobe techniques to the Sri Lanka zircon (LGC-1). We obtained twenty-two (U-Th)/He ages on nine shards using the laser microprobe method, showing an average (U-Th)/He age of 471.1 ± 16.6 Ma (1σ). This result is generally consistent with the mean conventional age (484.1 ± 9.6 Ma) for twenty-two zircon fragments. Both are nearly equal to the age value (~476 Ma) predicted by the He diffusion model and the thermal history model of Sri Lanka highland. The variations in the laser microprobe-derived ages are most likely caused by the uncertainties in volume measurements, which is also common in other studies. We used the Mahalanobis distance technique to reduce the volume measurement bias by identifying and eliminating abnormal data.
推进(U-Th)/He 锆石定年:样品制备和减少不确定性的新方法
激光微探针(U-Th)/He 测年法是一种高效的新技术,它利用了一套可互操作的集成仪器,包括准分子激光系统、四极杆氦质谱仪和四极杆电感耦合等离子体质谱仪。为了证明这种新方法的适用性,我们对斯里兰卡锆石(LGC-1)采用了传统和激光微探针技术。我们利用激光微探针方法在九块碎片上获得了 22 个 (U-Th)/He 年龄,显示平均 (U-Th)/He 年龄为 471.1 ± 16.6 Ma (1σ)。这一结果与二十二块锆石碎片的平均常规年龄(484.1 ± 9.6 Ma)基本一致。两者都几乎等于斯里兰卡高地氦扩散模型和热历史模型预测的年龄值(~476 Ma)。激光微探针年龄的变化很可能是由于体积测量的不确定性造成的,这在其他研究中也很常见。我们采用了马哈拉诺比斯距离技术,通过识别和剔除异常数据来减少体积测量的偏差。
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来源期刊
Lithosphere
Lithosphere GEOCHEMISTRY & GEOPHYSICS-GEOLOGY
CiteScore
3.80
自引率
16.70%
发文量
284
审稿时长
>12 weeks
期刊介绍: The open access journal will have an expanded scope covering research in all areas of earth, planetary, and environmental sciences, providing a unique publishing choice for authors in the geoscience community.
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