Abstract
This paper deals with the geological structure of the Amur zinc deposit. The host shaly-carbonaceous flysch sediments are evaluated from the point of view of their precious metal, tungsten, and molybdenum potential. It is shown that the rare-metal mineralization is superimposed on a primarily sedimentary precious-metal mineralization and stratiform zinc ores. The discussed data permit us to look at these carbonaceous sediments as highly prospective for rare metal and precious metal mineralization.
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