Abstract：The baiyun gold deposit is a polygenetic and mixedhydrothermal deposit controlled by reverse-thrust faults in the Liaohe group of Fengcheng county of eastern Liaoning. The metallic mineral constitution of the ore is simple, and the pyrite is the most principal Au-bearing mineral,its proportion in the metal minerals is up to 92%. On the basis of mineralization features of the deposit, the authors systematically determined and analysed the special physical property, chemical composition, geochemical and S-isotopic characters of the pyrite collected respectively from the formal wallrocks, i.e. metamorphic rocks, mineralized direct wallrocks, i.e. K-silicified.altered rocks and various ore types, then studied the typomorphic charcterictics of the pyrite and made an inquiry into its genesis and exploration significance.
国家辉, 程德琳. 辽宁白云金矿床黄铁矿标型特征及其找矿意义[J]. 地质与资源, 1993, 2(2): 127-136.
Guo Jiahui, Cheng Delin. TYPOMORPHIC CHARACTERISTICS OF THE PYRITE IN BAIYUN GOLD DEPOSIT AND THEIR SIGNIFICANCE TO EXPLORATION OF THE DEPOSIT. GEOLOGY AND RESOURCES, 1993, 2(2): 127-136.
1993, Vol. 2 
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