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Economic Geology; October 1968; v. 63; no. 6; p. 694-695
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Calaverite at Vatukoula, Fiji

D. L. Forsythe

The presence of calaverite in ore specimens has been confirmed by x-ray diffraction, confirming the conclusion of L. J. Cabri (1965), from experimental work, that calaverite-krennerite assemblages should be stable at fairly low temperatures.

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