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苏联某含金硫化物矿床产于上元古界沉积变质的黑色页岩建造中.该区金矿有两种类型:含金硫化物建造和含金石英脉建造.根据矿物共生组合,矿化可划分为三个阶段,第二阶段是金矿化的主要阶段.??维库洛娃等对该区的矿物进行了深入细致的综合研究,认为各个矿物共生组合都有其结构,构造和矿物学特点,并且有相应的具有其标型特征的黄铁矿.
A gold-bearing sulphide deposit in the Soviet Union originated in the construction of black shale in the Proterozoic metamorphic sedimentary deposits, where gold deposits are of two types: gold-bearing sulphides and gold-bearing quartz veins. According to mineralogical assemblages, mineralization Can be divided into three stages, the second stage is the main stage of gold mineralization.Vikurova and other minerals in the area conducted a comprehensive and detailed study that each of the various mineral assemblages have their structure, structure and Mineralogical characteristics, and have the corresponding pyrite with its standard features.