Discussion – Paleoplacers of the Witwatersrand Basin – Mining Engineering, Vol. 42, No. 2, pp. 195-199 – Minter, W. E. L.

Society for Mining, Metallurgy & Exploration
E. S. Cheney
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Society for Mining, Metallurgy & Exploration
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361 KB
Publication Date:
Jan 1, 1991

Abstract

Minter (1990) has provided an excellent summary of the sedimentology and theories of origin of the Witwatersrand paleoplacer Au/U deposits. However, recent stratigraphic, metamorphic and structural-tectonic research is radically changing the concepts about the Witwatersrand that now occur in most textbooks, review articles and North American minds. Presently, these concepts are biased by the past sedimentological research so well described by Minter. Specifically, the Witwatersrand Supergroup is Archean, does not occupy a depositional basin and is significantly metamorphosed and deformed. Thus, many of its sedimentary features, including the mineralogy of its ores, have been modified. The importance of the Witwatersrand ores cannot be overestimated. Since their discovery in 1886, they have produced 52% of the gold mined in all of human history (Pretorius, 1989).
Citation

APA: E. S. Cheney  (1991)  Discussion – Paleoplacers of the Witwatersrand Basin – Mining Engineering, Vol. 42, No. 2, pp. 195-199 – Minter, W. E. L.

MLA: E. S. Cheney Discussion – Paleoplacers of the Witwatersrand Basin – Mining Engineering, Vol. 42, No. 2, pp. 195-199 – Minter, W. E. L.. Society for Mining, Metallurgy & Exploration, 1991.

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