Issue 8, 2022

A natural plagioclase reference material for microbeam Sr isotopic analysis

Abstract

High-quality Sr isotope data are critically dependent on the quality of reference materials that are used for instrumental calibration and data monitoring during LA-MC-ICP-MS analysis. A suite of natural plagioclase samples (BDL-1, BDL-2 and BDL-3) from the Badaling intrusive complex, Beijing were investigated here to test their suitability as a plagioclase Sr isotope reference material. Major and trace element analyses by EPMA and LA-ICP-MS showed that plagioclase crystals separated from two troctolites (BDL-1 and BDL-3) and one gabbro (BDL-2) were all characterized by extremely low Rb/Sr ratios (0.00012–0.00047), and low heavy rare earth elements (HREEs) and high Sr contents (2377–2836 μg g−1). A total of 200 LA-MC-ICP-MS analyses for plagioclases BDL-1, BDL-2 and BDL-3 showed consistent and homogeneous Sr isotopic compositions with an average 87Sr/86Sr ratio of 0.70535 ± 0.00007 (2SD), which was in good agreement with solution-based data determined by TIMS or SN-MC-ICP-MS (0.70533 ± 0.00004; 2SD, n = 12), thus suggesting that BDL plagioclase can be used as a potential reference material for microbeam Sr isotopic analysis. Compared to the other available plagioclase Sr isotopic reference materials, the large quantities, long-term availability, high Sr content and extremely low isobaric interference (Rb, Er and Yb) of BDL plagioclase make it especially suitable for instrumental calibration and to adjust for inter-laboratory bias of the measured 87Sr/86Sr ratios.

Graphical abstract: A natural plagioclase reference material for microbeam Sr isotopic analysis

Supplementary files

Article information

Article type
Paper
Submitted
31 Mar 2022
Accepted
07 Jun 2022
First published
13 Jun 2022

J. Anal. At. Spectrom., 2022,37, 1706-1714

A natural plagioclase reference material for microbeam Sr isotopic analysis

L. Xu, J. Yang, H. Wang, Y. Li, B. Zhou, Y. Yang, C. Huang, L. Xie and S. Wu, J. Anal. At. Spectrom., 2022, 37, 1706 DOI: 10.1039/D2JA00110A

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