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Economic Geology; February 1968; v. 63; no. 1; p. 85-86
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Two varieties of pyrite from the Basal Reef of the Witwatersrand system [discussion]

S. H. U. Bowie

Anisotropy in pyrite was shown by R. Saager and P. Mihalik to be due to trace-metal content (for reference, see this Bibliography Vol. 32, No. 4, 11 E68-04487), but can have other causes. 'The same crystal of pyrite in different orientations can be polished so that it appears either isotropic or anisotropic.'

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