Therefore, the fractal cluster dimension and fractal density dimension can be used as the quantitative indicators of deposits distribution, intensity of mineralization and accumulation.
因此，分形丛集维数和分形密集维数可以作为矿床分布、矿化强度和聚集的定量指标。
Statistical distribution parameters are varied at different positions of mineralized bodies which reflects variation of mineralization intensity in the vertical extent.
矿化体在不同部位上的统计分布参数不同，反映了垂向空间上矿化强度的变化。
Combination of tectonic deformation and tectonic rocks in structural belts controls type, intensity and location of mineralization and alteration.
断裂带内构造变形强度和构造岩的类型及性质组合控制了矿化和蚀变的类型、强度及产出位置。
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