Hostname: page-component-857557d7f7-9f75d Total loading time: 0 Render date: 2025-11-22T03:51:00.580Z Has data issue: false hasContentIssue false
  • English
  • Français

Graphite in natural and experimental carbonate systems

Published online by Cambridge University Press:  14 March 2018

D. C. Gellatly
D. C. Gellatly*
Affiliation:
Research Institute of African Geology, Department of Geology, University of Leeds 1
Get access Rights & Permissions [Opens in a new window]

Summary

Graphite occurs in the Darkainle nepheline syenite complex, Somali Republic, as small drop-like grains in an altered ankeritic carbonatite; it has been recorded previously from carbonate-bearing nepheline syenites and kimberlites. Experimental evidence indicates that siderite decomposes to a stable association of magnetite and graphite within the PT ranges 500 to 10 000 bars and 455 to 745° C. The graphite in carbonatite and other alkaline igneous rocks may have been formed similarly by the decomposition of siderite or iron-rich carbonates.

Information

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 35 , Issue 275 , September 1966 , pp. 963 - 970
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1966

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

Article purchase

Temporarily unavailable

References

Adams, (F. D.) and Barlow, (A. E.), 1910. Mere. Geol. Surv. Canada, no. 6.Google Scholar
Bardet, (M. G.), 1965. Econ. Geol., vol. 60, p. 827.Google Scholar
Davidson, (C. F.), 1964. Ibid., vol. 59, p. 1368.Google Scholar
Dawson, (J. B.), 1960. Ph.D. Thesis, University of Leeds.Google Scholar
Dawson, (J. B.), 1962. Bull. Geol. Soc. Amer., vol. 73, p. 545.Google Scholar
Eckermann, (H. VON), 1948. Sver. Geol. Undersök., 36. [M.A. 11-27].Google Scholar
Eckermann, (H. VON), 1961. Bull. Geol. Inst. Univ. Uppsala, vol. 40, p. 25.Google Scholar
French, (B. M.) and Rosenberg, (P. E.), 1965. Science, vol. 147, p. 1283.Google Scholar
Garson, (M. S.), 1962. Mere. Geol. Surv. Nyasaland, no. 2.Google Scholar
Garson, (M. S.) and SMITH (W. CAMPBELL), 1958. Ibid., no. 1.Google Scholar
Gellatly, (D. C.), 1963a. Ann. Rept. Res. Inst. African Geol., Univ. Leeds, no. 7, p. 15.Google Scholar
Gellatly, (D. C.), 1963b. Ph.D. Thesis, Univ. Leeds.Google Scholar
Gittins, (J.), 1961. Journ. Geol., Chicago, vol. 69, p. 291. [M.A. 15-557].Google Scholar
Higazy, (R. A.), 1954. Bull. Geol. Soe. Amer., vol. 65, p. 39. [M.A. 12-380].Google Scholar
Holland, (T. H.), 1901. Mem. Geol. Surv. India, vol. 30, p. 199.Google Scholar
Holmes, (A.), 1937. Trans. Geol. Soc. South Africa, vol. 39 (for 1936), p. 379. [M.A. 7-187].Google Scholar
Holmes, (A.), 1950. Amer. Min., vol. 35, p. 722.Google Scholar
[Kupletsky, (B. M.)] , 1925, in [Yakhontov, (N.)] (H.) et al., [Materials to the knowledge of Russian Graphite], no. 55 of CCCP [Materials for a knowledge of the natural productive forces, USSR], Leningrad [abstr. in M.A. 3-74].Google Scholar
Nixon, (P.), von Knorring, (O.), and Rooke, (J. M.), 1963. Amer. Min., vol. 48, p. 1090.Google Scholar
Noda, (T.) and Matsuoka, (H.), 1960. [Journ. Chem. Soe. Japan, vol. 63, p. 465]. abstr, in M.A. 15-3.Google Scholar
Powell, (H. E.), 1965. U.S. Dept. Interior, Bur. Mines Rept. 6643.Google Scholar
Smirnov, (G. I.), 1959. Int. Geol. Review, vol. 1, p. 21. [M.A. 16-80].CrossRefGoogle Scholar
Wlidner, (J. R.) and Tuttle, (O. F.), 1965. Geol. Soc. Amer., Special Paper no. 82, p. 220.Google Scholar
Williams, (A. F.), 1932. The Genesis of the Diamond, Benn (London).Google Scholar
Wyllie, (P. J.) and Tuttle, (O. F.), 1959a. Nature, vol. 183, p. 770. [M.A. 14-334].Google Scholar
Wyllie, (P. J.) and Tuttle, (O. F.), 1959b. Anler. Min., vol. 44, p. 453. [M.A. 14-334].Google Scholar
Wyllie, (P. J.) and Tuttle, (O. F.), 1960. Journ. Petr., vol. 1, p. 1. [M.A. 14-406].CrossRefGoogle Scholar