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.
并应用饱和指数的找矿机理，对测老庙盆地的找矿前景提出了水文地球化学依据。
Moreover, hydrogeochemical basis for the prospecting potential of the Celaomiao Basin is presented on the basis of the prospecting mechanism of saturation index.
秦岭地区的岩体铁指数相对较低，只有0.62，岩石成因类型的地球化学判据既有A型也有I型花岗岩特征。
The Fe content of Qinling rock body is relatively lower, only 0.62. The petro-geochemical for determining the genesis not only has A-type, but also has I-type granite characteristics.
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