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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.
利用已知矿床的原生晕和元素的分带性确定了成矿的地球化学特征,提出叠加型异常是该区找矿的重要靶区。
The ore-forming geochemical characteristics were confirmed according to the primary halos and elements zoning of known deposits. The imposed anomaly was the important prospecting targets in the area.
利用滑轮部分带动整个沙发运动。
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