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通过对高松山金矿床特征、地球化学特征的分析研究,认为高松山金矿床为浅成低温热液型金矿床,成矿地层是甘河期火山岩,以亚碱性系列之钙碱性高钾火山岩为特征。火山岩稀土元素分析结果表明,该火山岩属轻稀土富集型,铕无明显异常,稀土配分曲线为平缓的右倾。岩石微量元素曲线形态基本相似,表明岩浆具有同源特点。火山岩成因类型为壳-壳幔活动大陆边缘的产物。岩浆演化以分异作用为主,并受一定陆壳混染。
Based on the analysis of the characteristics and geochemical characteristics of the Takamatsu Gold Deposit, it is concluded that the Takamatsu Gold Deposit is a epithermal-type gold deposit, and the metallogenic strata are volcanic rocks in the Ganhe Period. Calcium-alkaline potassium Volcanic rocks are featured. The results of REE analysis of volcanic rocks show that the volcanic rocks belong to the light rare earth enrichment type, while the europium shows no obvious anomaly. The distribution curve of rare earth elements is a gentle rightward dip. The curve of trace elements in rock is basically similar, indicating that magma has the same origin. The type of volcanic rocks is the product of the active continental margin of the crust-mantle. The evolution of magma is dominated by differentiation and is contaminated by some continental crust.