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霍州矿区断层构造的分形特征与渭河盆地东区基本相同,都形成于张扭性的动力学环境;矿区内各井田的断层分维值以白龙井田最高,团柏井田最低;分维值的大小体现断层构造的复杂程度。
The fractal features of the fault structure in Huozhou Mine Area are basically the same as those in the eastern Weihe Basin and are formed in a dynamic environment with tension and torsion. The fractal dimension values of each mine field are the highest in Bailong Minefield and the lowest in Tubaai Minefield; the fractal values Size reflects the complexity of the fault structure.