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Economic Geology; January 1940; v. 35; no. 1; p. 98-108
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Developments on and around the Witwatersrand

Alexander L. Du Toit

Presents a detailed analysis of the nature and origin of the gold deposits. The auriferous bodies form surprisingly constant layers of mineralized conglomerate called "Banket" averaging between 2 and 7 feet in thickness. Two theories of origin have been advanced, placer and hydrothermal.

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