The experiments were carried out in the system 6N HC1 aqueous solution-synthetic Au-Ag alloys with various Ag/Au ratios in order to investigate the dissolution and precipitation of gold and silver at 150°C over a period of 120 days. Pure gold precipitate was formed in run #3(Au
50Ag
50), #4(Au
75Ag
25) and #5(Au
90Ag
10), in which the Ag/Au atomic ratio in solution was less than 1. Gold-silver alloy (electrum) was formed in run #1(Au
10Ag
90) and #2(Au
25Ag
75), in which the Ag/Au atomic ratios in solution were about 330 and 670, respectively. Assuming that gold and silver chloro-complexes are dominant in ore fluids, Ag/Au atomic ratios in ore fluids for the Transbaykalial gold deposits and the Japanese auriferous hydrothermal vein deposits are calculated and estimated to lie in the range of 7 to 690.
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