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Siniukhinskoe地区Veselyi矿床的矿化产于矽卡岩的内外接触带中,围岩为古生代的火山熔岩、凝灰岩和夹层灰岩。矽卡岩的形成与闪长岩墙群的侵入有关。Cu-Au矿化的产生和矽卡岩的退化蚀变过程相联系。成矿热液是岩浆成因的热卤水与大气降水的混合流体。
The mineralization of the Veselyi deposit in the Siniukhinskoe region occurs in the inner and outer contact zones of the skarn. The surrounding rock is Paleozoic volcanic lava, tuff and disseminated limestone. The formation of skarn is related to the intrusion of diorite wall group. The Cu-Au mineralization is linked to the degenerated alteration of skarn. Mineralization hydrothermal fluid is a mixed fluid of magmatic hot brine and atmospheric precipitation.