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Direct evidence of present-day serpentinization in the Jimberlana Intrusion, Western Australia

Published online by Cambridge University Press:  01 May 2009

I. H. Campbell
I. H. Campbell
Affiliation:
Department of GeologyUniversity of MelbourneParkville, VictoriaAustralia3052
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Summary

Four vertical holes drilled into the olivine cumulates of the Jimberlana Intrusion all show a decrease in serpentinization with depth, suggesting that serpentinization can be a low temperature, present-day process.

Type
Articles
Information
Geological Magazine , Volume 112 , Issue 1 , January 1975 , pp. 77 - 80
Copyright
Copyright © Cambridge University Press 1975

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References

Barnes, I., La Marchie, V. C. & Himmelberg, G. 1967. Geochemical evidence of present-day serpentinization. Sci. 156, 830–2.CrossRefGoogle ScholarPubMed
Barnes, I. & O'Neil, J. R. 1969. The relationship between fluids in some fresh alpine-type ultramafics and possible modern serpentinization, Western U.S. Bull. geol. Soc. Am. 80, 1947–59.CrossRefGoogle Scholar
Campbell, I. H., McCall, G. J. H. & Tyrwhitt, D. S. 1970. The Jimberlana Norite, Western Australia – a smaller analogue of the Great Dyke of Rhodesia. Geol. Mag. 107, 1–12.CrossRefGoogle Scholar
Coleman, R. G. & Keith, T. E. 1971. A chemical study of serpentinization – Burro Mountain, California. J. Petrology 12, 311–28.CrossRefGoogle Scholar
Johannes, W. 1969. An experimental investigation of the system MgO–SiO2–H2O–CO2. Am. J. Sci. 267, 1083–104.CrossRefGoogle Scholar
Worst, B. G. 1960. The Great Dyke of Southern Rhodesia. Bull. S. Rhod. geol. Surv. 47, 234 pp.Google Scholar