The stability of graphite and diamond as a function of the oxygen fugasity in the mantle

E. Woermann; B. Knecht; M. Rosenhauer; G.C. Ulmer

doi:10.29173/ikc1048

The stability of graphite and diamond as a function of the oxygen fugasity in the mantle

Authors

E. Woermann
B. Knecht
M. Rosenhauer
G.C. Ulmer

DOI:

https://doi.org/10.29173/ikc1048

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Published

1977-09-12

How to Cite

Woermann, E., Knecht, B., Rosenhauer, M., & Ulmer, G. (1977). The stability of graphite and diamond as a function of the oxygen fugasity in the mantle. International Kimberlite Conference: Extended Abstracts, 2(1), 358–359. https://doi.org/10.29173/ikc1048

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Issue

Vol. 2 (1977): Vol 2: International Kimberlite Conference, Santa Fe

Section

Extended Abstracts

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