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通过对侯马紫金山一带成矿地质背景,赫家山金矿矿体地质等的综合分析,认为其成因类型属中低温热液型,矿体受北北东向及北北西向晚期次级断裂构造的控制,并对矿床成因及形成机制进行了初步分析。
Through the comprehensive analysis of the metallogenic geological background of the Houma Zijin Mountain and the orebody geology of the Hejiashan Gold Mine, it is considered that the genetic type belongs to the low-temperature hydrothermal type. The ore body is affected by the north-north eastward and the north-northwestward Tectonic control, and a preliminary analysis of the genesis and formation mechanism of the deposit.