JOURNAL ARTICLE
First Determination of δ53CrSRM979 in Sixteen Geological Reference Materials Using Double Spike Thermal Ionisation Mass Spectrometry after a Two‐Column Matrix Separation.
Published In: Geostandards & Geoanalytical Research, 2025, v. 49, n. 3. P. 537 1 of 3
Database: Academic Search Ultimate 2 of 3
Authored By: Wei, Yuqiu; Zhou, Lian; Hu, Anping; Cheng, Jie; Hu, Qiankun; Shen, Anjiang; Hu, Yating; Feng, Lanping 3 of 3
Abstract
We report for the first time δ53CrSRM 979 values in sixteen geological reference materials (RMs) with varied lithological characteristics. The measured values range from ‐0.24‰ ± 0.05‰ (2s) to ‐0.08‰ ± 0.02‰ (2s) for igneous rocks, from ‐0.18 ± 0.04‰ (2s) to 0.08 ± 0.03‰ (2s) for sedimentary rocks and between ‐0.21‰ ± 0.04‰ (2s) and ‐0.10‰ ± 0.04‰ (2s) for metamorphic rocks, indicating significant isotopic fractionation across these RMs. Measurements were performed using thermal ionisation mass spectrometry with a 50Cr‐54Cr double‐spike technique following a two‐column matrix separation. To validate our measurement procedure, we applied it to eighteen additional well‐characterised RMs. Our results are in agreement with previously reported values, with precision typically below 0.05‰ (2s). This comprehensive data set provides a valuable reference for quality assurance schemes and inter‐laboratory comparisons in Cr isotopic studies. [ABSTRACT FROM AUTHOR]
Additional Information
- Source:Geostandards & Geoanalytical Research. 2025/09, Vol. 49, Issue 3, p537
- Document Type:Article
- Subject Area:Science
- Publication Date:2025
- ISSN:1639-4488
- DOI:10.1111/ggr.12610
- Accession Number:188363341
- Copyright Statement:Copyright of Geostandards & Geoanalytical Research is the property of Wiley-Blackwell and its content may not be copied or emailed to multiple sites without the copyright holder's express written permission. Additionally, content may not be used with any artificial intelligence tools or machine learning technologies. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)
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