Abstract
THIS communication summarizes the principal results obtained from a detailed petrological, mineragraphic and chemical study of the concordant type No. 7 lead–zinc orebody, Mount Isa, and the host shales which constitute the Urquhart Formation, usually referred to as the Urquhart shales1.
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References
Croxford, N. J. W., doctorate thesis, University of New England (1962).
Blanchard, R., and Hall, G., Proc. Austral. Inst. Min. Metall., 125, 1 (1942).
Croxford, N. J. W., Trans. Inst. Min. Metall., 74, 33–43 (1964–65).
Carter, S. R., Fifth Emp. Min. Metall. Congr., 1, 361 (1953).
Murray, W. J., Proc. Austral. Inst. Min. Metall., 197, 105 (1961).
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CROXFORD, N. Sulphide-sediment Relationships at Mount Isa. Nature 206, 1144–1145 (1965). https://doi.org/10.1038/2061144b0
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DOI: https://doi.org/10.1038/2061144b0
