Abstract
Typomorphic features of native gold from two placers of the Tarlau area were studied. It was demonstrated that migration of the gold particles had been proceeded both through transition to lower hypsometric levels in the weathering crust and during transportation by water flows. The complex of the studied features allows one to testify for the gold deposition within a single stage of the ore process, to suggest that the primary source was represented by a gold-sulfide-quartz type occurrence, and to assign the Tarlau and Murin placers to the origin section of the scattering zone of a unified placer.
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