原生晕分析是研究矿床深部矿化远景的有效手段。
Primary halo is very effective to detect the deep mineralization of ore deposits.
运用回归分析，模拟出原生金矿化元素地球化学模型。利用变异性指数法确定了矿体原生晕垂向分带。
Element geochemistry model of the primary mineralization halo is simulated by regression analysis and vertical zoning of the ore body primary halo by variable index method.
总结了金矿床地球化学异常模式和原生晕分带序列的研究成果。针对我国化探找金提出了一些设想和建议。
The author sums up the studies of geochemical anomaly pattern and primary halo zoning sequence of gold deposits, and makes some Suggestions as a guide for future gold exploration work in China.
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