High-precision Fe isotope analysis for low contents using a Nu Sapphire instrument
Iron (Fe) isotopes serve as a powerful tracer for studying planetary evolution, magmatic processes, redox conditions, biological activities, and other key geological processes.
Authors
- Yingliang Cheng (ORCID: https://orcid.org/0000-0001-5809-4378)
- Xiaoyan Gu (ORCID: https://orcid.org/0000-0002-7419-1626)
- Jia Liu (ORCID: https://orcid.org/0000-0003-4949-6679)
- Qunke Xia (ORCID: https://orcid.org/0000-0003-1256-7568)
- Q J Ying (ORCID: https://orcid.org/0000-0001-7276-3793)
- Shenghua Zhou (ORCID: https://orcid.org/0000-0002-0335-4408)
- Jinjun Zhou (ORCID: https://orcid.org/0000-0002-6654-6466)
- Kai Yang (ORCID: https://orcid.org/0009-0004-7586-8856)
- Hong-Fu Zhang (ORCID: https://orcid.org/0009-0000-3776-4854)
- Xiaorong Wei (ORCID: https://orcid.org/0009-0000-2746-5391)
Institutions
- Planetary Science Institute (US)
Publication Details
- Journal
- Journal of Analytical Atomic Spectrometry
- Published
- 2025-01-01
- DOI
- https://doi.org/10.1039/d5ja00225g
- Citations
- 1
- Primary Topic
- Astro and Planetary Science
- Type
- article
- Field-Weighted Citation Impact
- 1.15