Crossmark

Ultra-reducing conditions in average mantle peridotites and in podiform chromitites: a thermodynamic model for moissanite (SiC) formation

Crossref DOI link: https://doi.org/10.1007/s00410-016-1253-9

Published Online: 2016-04-18

Published Print: 2016-05

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

Authors

Golubkova, Anastasia

Schmidt, Max W.

Connolly, James A. D.
Funding

Funding for this research was provided by:

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung (200020-140541/1)

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung (200020-153112/1)
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