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В.И.Смирнов和М.Б.Бородаевский等的研究表明,黄铁矿省矿床的现今面貌是由热液交代作用和热液-沉积作用相互造成的成矿物质的堆积所决定的。被研究矿床在成因上属于有争议的类型。В.П.Дмитриев等发展了矿床硫化物矿石属
Studies by В.И.Смирнов and М.Б.Бородаевский have shown that the present appearance of the pyrite deposits is determined by the accumulation of metallogenic materials that result from hydrothermal metasomatism and hydrothermal-sedimentation interactions. The studied deposit is genetically attributable to the disputed type. В.П.Дмитриев et al. Developed a deposit of sulphide ore