Abstract

The Golets Vysochaishii deposit is a sub-tabular ore body hosted by black carboniferous fine-grained aleuropelitic rocks. Fluid inclusions were studied in quartz samples collected from sulfide–quartz veins in the ore zone of the deposit. The studies provided the parameters of the ore-forming fluid. Fluids of the deposit were characterized by typical features of ore-forming fluids of the orogenic vein gold deposits. The precipitation of native gold in ores may have been stimulated by the process of carbon dioxide degassing from the fluid.

中文翻译：

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俄罗斯博代博区Golets Vysochaishii矿床金成矿条件新资料

摘要

Golets Vysochaishii 矿床是一个以黑色石炭系细粒胶泥质岩石为主体的亚板状矿体。研究了从矿床矿石带的硫化物-石英脉中采集的石英样品中的流体包裹体。这些研究提供了成矿流体的参数。矿床流体具有典型的造山脉金矿成矿流体特征。矿石中天然金的沉淀可能是受到流体中二氧化碳脱气过程的刺激。