Olivine and Fe-isotopes in kimberlites indicate an iron-rich substrate for CLIPPIR and other sub-lithospheric diamonds

Journal:

Nature Communications

Published:

2026-04-19

DOI:

10.1038/s41467-026-72060-0

Affiliations:

5

Authors:

5

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Institutions	Authors	Share
University of Cape Town (UCT), South Africa	2.000000	0.40
State Key Laboratory of Geological Processes and Mineral Resources, China	1.333333	0.27
Earth and Planets Laboratory, CIS, United States of America (USA)	1.000000	0.20
Macquarie University, Australia	0.333333	0.07
Australian National University (ANU), Australia	0.333333	0.07

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