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Redox state of the Dharwar craton root as inferred from eclogite and peridotite sourced mantle cargo, with implications for kimberlite and lamproite magma formation

Crossref DOI link: https://doi.org/10.1007/s00410-023-02072-2

Published Online: 2023-11-16

Published Print: 2023-12

Update policy: https://doi.org/10.1007/springer_crossmark_policy

Authors

Shaikh, Azhar M. https://orcid.org/0000-0002-7327-5414
Bussweiler, Yannick https://orcid.org/0000-0002-8107-7055
Viljoen, Fanus https://orcid.org/0000-0002-9640-6886
Bolhar, Robert https://orcid.org/0000-0003-3329-0262
Ravi, S.

Hezel, Dominik C. https://orcid.org/0000-0002-5059-2281
Ueckermann, Henriëtte https://orcid.org/0000-0003-1463-4031
Tappe, Sebastian https://orcid.org/0000-0003-1224-5155
Funding

Funding for this research was provided by:

DSI-NRF Centre of Excellence for Integrated Mineral and Energy Resource Analysis (93208)

University of Johannesburg

Department of Science and Innovation, South Africa (64779)

National Research Foundation (93208)
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Text and Data Mining valid from 2023-11-16

Version of Record valid from 2023-11-16
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Article History

Received: 2 March 2023

Accepted: 23 October 2023

First Online: 16 November 2023

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