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Pyrrhotine and the origin of terrestrial diamonds

Published online by Cambridge University Press:  05 July 2018

Paul C. Marx*
Affiliation:
Aerospace Corporation, El Segundo, California

Abstract

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Type
Short Communications
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1972

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References

Bundy, (F.P.), Bovenkerk, (H.P.), Strong, (H.M.), and Wentore, (R. H., Jr.), 1961. Journ. Chem. Phys. 35, 383-91.CrossRefGoogle Scholar
Clark, (S.P.) and Ringwood, (A.E.), 1964. Rev. Geophys. 2, 35-88.CrossRefGoogle Scholar
Hearn, (B. C., Jr.), 1968. Science, 159, 622- 5.CrossRefGoogle Scholar
Kennedy, (G.C.) and Nordlie, (B.E.), 1968. Econ. Geol. 63, 495-503.CrossRefGoogle Scholar
Lipschutz, (M.E.) and Anders, (E.), 1961. Geochimica Acta, 24, 83-105.CrossRefGoogle Scholar
Nafziger, (R.H.) and Muan, (A.), 1967. Amer. Min. 52, 1364-85.Google Scholar
Robie, (R.A.) and Waldbaum, (D.R.), 1968. Thermodynamic properties of minerals and related substances at 298.15 °K and one atmosphere and at higher temperatures. U.S. Geol. Surv. Bull. 1259.Google Scholar
Shand, (S.J.), 1952. Rocks for chemists. New York (Pitman).Google Scholar
Sharp, (W.E.), 1966. Nature, 211, 402- 3.CrossRefGoogle Scholar