Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-24T17:48:19.083Z Has data issue: false hasContentIssue false

On the occurrence of smolyaninovite in the Mount Cobalt deposit, in north-western Queensland, Australia

Published online by Cambridge University Press:  05 July 2018

L. K. Smith
Affiliation:
Department of Chemical Engineering, Monash University, Clayton, Victoria, 3168, Australia
K. N. Han
Affiliation:
Department of Chemical Engineering, Monash University, Clayton, Victoria, 3168, Australia
F. Lawson
Affiliation:
Department of Chemical Engineering, Monash University, Clayton, Victoria, 3168, Australia

Summary

Smolyaninovite, (Co, Ni, Ca, Mg)3 (Fe, Al)2 (AsO4)4. 11H2O, has recently been recognized in the mineralized region around Mount Cobalt, Queensland. It is a soft polycrystalline earthy yellow-brown material, is probably the weathering product of cobaltian arsenopyrite or alloclase, and shows para-magnetic properties.

Type
Research Article
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.)

Footnotes

1

Present address: I.C.I. Central Research Laboratories, Ascot Vale, Victoria, 3032, Australia.

References

Croxford, (N. J. W.), 1974. Mineral. Deposita, 9, 105–15.CrossRefGoogle Scholar
Rayner, (E. O.), 1953. 5th Empire Mining and Metallurgical Congress, 1, 417–25.Google Scholar
Yakhontova, (L. K.), 1956. Dokl. Akad. Nauk S.S.S.R. 109, 849–50.Google Scholar
Yakhontova, (L. K.), Sidorenko, (G. A.), Sergeeva, (N. E.), and Rybakova, (L. I.), 1973. Konst. Svoistva Mineral. 7, 120–3.Google Scholar