Bridgmanite’s ferric iron content determined Earth’s oxidation state
- DOI
- 10.1038/s41561-025-01725-0
- Published
- 2025-06-23
- Container
- Nature Geoscience
- Publisher
- Springer Science and Business Media LLC
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.1038/s41561-025-01725-0,
title = {Bridgmanite’s ferric iron content determined Earth’s oxidation state},
author = {Fei Wang and Lin Wang and Hongzhan Fei and Nobuyoshi Miyajima and Catherine McCammon and Daniel J. Frost and Tomoo Katsura},
year = {2025},
journal = {Nature Geoscience},
doi = {10.1038/s41561-025-01725-0},
url = {https://doi.org/10.1038/s41561-025-01725-0}
}RIS
TY - JOUR TI - Bridgmanite’s ferric iron content determined Earth’s oxidation state AU - Fei Wang AU - Lin Wang AU - Hongzhan Fei AU - Nobuyoshi Miyajima AU - Catherine McCammon AU - Daniel J. Frost AU - Tomoo Katsura PY - 2025 JO - Nature Geoscience DO - 10.1038/s41561-025-01725-0 UR - https://doi.org/10.1038/s41561-025-01725-0 ER -
APA
Wang, F., Wang, L., Fei, H., Miyajima, N., McCammon, C., Frost, D. J., & Katsura, T. (2025). Bridgmanite’s ferric iron content determined Earth’s oxidation state. Nature Geoscience. https://doi.org/10.1038/s41561-025-01725-0
Source records
- crossref · retrieved 2026-09-25T14:47:01.336Z