Hostname: page-component-78c5997874-xbtfd Total loading time: 0 Render date: 2024-11-13T06:50:55.715Z Has data issue: false hasContentIssue false
  • English
  • Français

Serpentine minerals from two areas of the Western Australian nickel belt

Published online by Cambridge University Press:  05 July 2018

P. G. Moeskops
Get access Rights & Permissions [Opens in a new window]

Summary

Investigation of serpentine minerals from metaserpentinized ultramafic rocks in two Archaean green-stone belts, east of Kalgoorlie, has indicated that antigorite, exhibiting a very wide range of textures in thin section, is the dominant serpentine species; however, it is locally accompanied by relict lizardite. Chrysotile occurs both in late tectonic veins and as a present-day weathering product of relict olivine. Analytical data and structural formulae on seven serpentines, characterized independently by X-ray diffraction analysis, support the chemical differences between antigorite and chrysotile postulated by earlier workers.

Type
Research Article
Information
Mineralogical Magazine , Volume 41 , Issue 319 , September 1977 , pp. 313 - 322
Copyright
Copyright © The Mineralogical Society of Great Britain and Ireland 1977

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.)

References

Barnes, (I. L.) and Himmelberg, (G.), 1967. Sci. 156, 830–2.CrossRefGoogle Scholar
Barnes, (I. L.) and O'Neil, (J. R.), 1969. Bull. Geol. Soc. Amer. 80, 1947-60.CrossRefGoogle Scholar
Basta, (E. Z.) and Kader, (Z. A.), 1969. Mineral. Mag. 37, 394–408.CrossRefGoogle Scholar
Campbell, (I. H.), 1976. Direct Evidence of Present-day Serpentinisation in the Jimberlana Intrusion, Western Australia (in prep.).Google Scholar
Cerny, (P.), 1968. Am. Mineral. 53, 1377-85.Google Scholar
Coats, (C. J.), 1967. Can. Mineral. 322-47.Google Scholar
Coleman, (R. G.) and Keith, (T. E.), 1971. J. Petrol. 12, 311–28.CrossRefGoogle Scholar
Deer, (W. A.), Howie, (R. A.), and Zussman, (J.), 1967. The Rock Forming Minerals. 4. Longmans, London.Google Scholar
Faust, (G. T.) and Fahey, (J. J.), 1962. U.S. Geol. Surv. Prof. Pap. 384A. Google Scholar
Green, (D. H.), 1961. Geol. Mag. 98, 1–26.CrossRefGoogle Scholar
Harker, (A.), 1950. Metamorphism. Methuen, London.Google Scholar
Hostetler, (B. P.), Coleman, (R. G.), Mumpton, (F. A.), and Evans, (B. W.), 1966. Am. Mineral. 51, 175–98.Google Scholar
Lauder, (W. R.), 1965. N.Z. J. Geol. Geophys. 8, 475–504.CrossRefGoogle Scholar
Moeskops, (P. G.), 1973. The Bulong Serpentinite and Environments of Nickel Mineralisation near Kdlgoorlie, Western Australia. Unpub. Lond. Univ. Ph.D. thesis.Google Scholar
Moeskops, (P. G.) and Nicholls, (I. A.), 1976. The Corsair Metaserpentinites, near Kdlgoorlie, Western Australia (in prep.).Google Scholar
Page, (N. J.), 1966. The Mineralogy and Chemistry of the Serpentine Group Minerals and the Serpentinisation Process. Unpub. Berkeley, Ph.D. thesis.Google Scholar
Spry, (A.), 1969. Metamorphic Textures. Oxford, Pergamon Press.Google Scholar
Wenner, (D. B.) and Taylor, (H. P.), 1971. Contr. Mineral. Petrol. 32, 165–85.CrossRefGoogle Scholar
Whittaker, (E. J. W.) and Wicks, (F. J.), 1970. Am. Mineral. 55, 1025-47.Google Scholar
Whittaker, (E. J. W.) and Wicks, (F. J.) and Zussman, (J.), 1956. Mineral. Mag. 31, 107–26.Google Scholar
Williams, (I. R.), 1969. Explanatory Notes on the Kurnalpi 1:250,000 Geological Sheet: West. Aust. Geol. Surv. Rec. (unpublished).Google Scholar
Worst, (B. G.), 1960. Bull. South. Rhodesian Geol. Surv. 47.Google Scholar