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以胶东望儿山断裂为例,通过断裂面形态的模拟,探讨已知矿体和断裂形态之间的关系,进而预测深部矿体可能赋存部位,这是一种直观、科学的预测方法。 ‘
Taking the Wangershan fault in Jiaodong as an example, the relationship between the known orebody and the fracture morphology is explored through the simulation of the fracture surface morphology, and then the possible occurrence of the deep orebody is predicted. This is an intuitive and scientific prediction method. ’