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

Downloads

PDF

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

Download Citation

Issue

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

Section

Extended Abstracts

Most read articles by the same author(s)

E. Woermann, M. Gobbels, G.C. Ulmer, D.E. Grandstaff, Moissanite and its bearing on the oxygen fugacity of the deeper regimes of the Earth's upper mantle , International Kimberlite Conference: Extended Abstracts: Vol. 7 (1998): Vol 7: International Kimberlite Conference, Cape Town
M. Rosenhauer, E. Woermann, B Knecht, C.G. Ulmer, The stability of graphite and diamond as a function of the oxygen fugasity in the mantle , International Kimberlite Conference: Extended Abstracts: Vol. 2 (1977): Vol 2: International Kimberlite Conference, Santa Fe
G.C. Ulmer, D.E. Grandstaff, M. Gobbels, E. Woermann, An experimental delineation of the oxygen fugacity of moissanite (SiC) bearing silicate systems , International Kimberlite Conference: Extended Abstracts: Vol. 7 (1998): Vol 7: International Kimberlite Conference, Cape Town
E. Woermann, M. Rosenhauer, Oxygen fugacity and the fluid C-H-O phase in the Earth’s mantle , International Kimberlite Conference: Extended Abstracts: Vol. 3 (1982): Vol 3: Third International Kimberlite Conference, Clermont-Ferrand