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辽宁处于华北地台北缘,地质历史漫长,矿化活动频繁。金矿的类型是比较复杂而多样的。在前人对金矿床的主要分类的基础上,结合岩金矿床的成矿作用、主要控矿因素、矿质来源、容矿岩石建造等方面的特征将金矿床划分为岩浆—热液金矿床、次火山—热液金矿床、沉积—变质金矿床、变质—热液金矿床等4个主要成因类型,并概括了各类型金矿床的成矿特征,以寻找到相似的矿床。
Liaoning is located in the northern margin of the North China Platform with a long geological history and frequent mineralization activities. The type of gold mine is more complex and diverse. Based on the previous classification of the gold deposits, the gold deposits are divided into magmatic-hydrothermal gold deposits based on the mineralization, the main ore-controlling factors, the mineral sources and the ore-bearing rocks. Sub-volcanic-hydrothermal gold deposits, sedimentary-metamorphic gold deposits, metamorphic-hydrothermal gold deposits, and summarizes the metallogenic characteristics of various types of gold deposits to find similar deposits.