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X-ray, optical, and morphological observations on hodgkinsonite from Franklin Furnace1

Published online by Cambridge University Press:  14 March 2018

W. M. B. Roberts  and
F. M. Quodling
W. M. B. Roberts
Affiliation:
Bureau of Mineral Resources, Geology, and Geophysics, Canberra, A.C.T., Australia
F. M. Quodling
Affiliation:
Department of Geology and Geophysics, The University of Sydney, Sydney, Australia
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Summary

Re-examination of hodgkinsonite by optical and X-ray methods has shown the desirability of adopting a setting different from that selected by Palache and Schaller and by Rentzeperis. In the new arrangement the b and c axes are interchanged and the original negative end of the b-axis becomes positive. A table of angles for the common forms is given, also X-ray powder data and a space group determination.

Type
Research Article
Information
Mineralogical magazine and journal of the Mineralogical Society , Volume 33 , Issue 259 , December 1962 , pp. 343 - 346
Copyright
Copyright © 1962, The Mineralogical Society

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References

Palache, (C.) and Scihaller, (W. T.), 1914. Zeits. Kryst. Min., vol. 53, p. 529.Google Scholar
Palache, (C.) 1914. Ibid., p. 675.Google Scholar
Palache, (C.) 1935. U.S. Geol. Survey Prof. Paper 180.Google Scholar
Rentzeperis, (P.J.), 1958.Acta Cryst., vol. 11, p. 448.CrossRefGoogle Scholar