Olivine and Fe-isotopes in kimberlites indicate an iron-rich substrate for CLIPPIR and other sub-lithospheric diamonds
- DOI
- 10.1038/s41467-026-72060-0
- Published
- 2026-04-19
- Container
- Nature Communications
- Publisher
- Springer Science and Business Media LLC
- Open access
- unknown
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Cite this work
BibTeX
@article{allodium:10.1038/s41467-026-72060-0,
title = {Olivine and Fe-isotopes in kimberlites indicate an iron-rich substrate for CLIPPIR and other sub-lithospheric diamonds},
author = {Geoffrey H. Howarth and Andrea Giuliani and Merrily M. Tau and Ronghua Cai and Jingao Liu},
year = {2026},
journal = {Nature Communications},
doi = {10.1038/s41467-026-72060-0},
url = {https://doi.org/10.1038/s41467-026-72060-0}
}RIS
TY - JOUR TI - Olivine and Fe-isotopes in kimberlites indicate an iron-rich substrate for CLIPPIR and other sub-lithospheric diamonds AU - Geoffrey H. Howarth AU - Andrea Giuliani AU - Merrily M. Tau AU - Ronghua Cai AU - Jingao Liu PY - 2026 JO - Nature Communications DO - 10.1038/s41467-026-72060-0 UR - https://doi.org/10.1038/s41467-026-72060-0 ER -
APA
Howarth, G. H., Giuliani, A., Tau, M. M., Cai, R., & Liu, J. (2026). Olivine and Fe-isotopes in kimberlites indicate an iron-rich substrate for CLIPPIR and other sub-lithospheric diamonds. Nature Communications. https://doi.org/10.1038/s41467-026-72060-0
Source records
- crossref · retrieved 2026-09-26T16:26:31.918Z