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本文简介了分形理论与经典测度间的某些区别。指出对形态复杂但结构具有标度不变性的矿床而言,用分形理论进行研究,比传统几何描述更为适宜,同时,还可据此,对矿床成因动力学作相关探讨。
This article describes some of the differences between the fractal theory and the classical measure. It is pointed out that fractal theory is more suitable than the traditional geometric description for the deposit with complex shape but scale invariance. Meanwhile, it can be used to discuss the genesis kinetics of the deposit.