Abstract
40Ar/39Ar datings of quartz-mica-sulfide, quartz-gold-arsenopyrite-pyrrhotite and quartz-gold-antimony associations at the ultra-large (more than 1000t. Au) Olimpiadinski gold deposit (Yenisei ridge) have been correlated. It was found that hydrothermal activity at the deposit lasted at least 150 ma.y. from 817 to 660 ma.y.
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