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Partitioning of Fe2O3 in peridotite partial melting experiments over a range of oxygen fugacities elucidates ferric iron systematics in mid-ocean ridge basalts and ferric iron content of the upper mantle

Crossref DOI link: https://doi.org/10.1007/s00410-021-01823-3

Published Online: 2021-08-12

Published Print: 2021-09

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

Authors

Davis, Fred A. http://orcid.org/0000-0002-5222-6330
Cottrell, Elizabeth
Funding

Funding for this research was provided by:

National Museum of Natural History (CGPS, Buck Fellowship)
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Text and Data Mining valid from 2021-08-12

Version of Record valid from 2021-08-12
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Article History

Received: 13 April 2021

Accepted: 26 July 2021

First Online: 12 August 2021

Change Date: 27 June 2022

Change Type: Correction

Change Details: A Correction to this paper has been published:

Change Details: https://doi.org/10.1007/s00410-022-01933-6

Updates are available Correction dated 2022-06-27

Click to view Correction: https://doi.org/10.1007/s00410-022-01933-6