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通过现场勘察发现，地质断裂面的几何形态表现为粗糙起伏的不规则性质，这种性质可以用分形几何学描述。以阜新矿区刘家沟Ｆ１号地质断裂露头为窗口，研究断裂面的分形性质，研究表明，断裂面具有各向异性分形特征。
Through on-site investigation, it is found that the geometry of the ruptured surface is irregular in roughness, which can be described by fractal geometry. Based on the outcrop of F1 geological fracture in Liujiagou of Fuxin Mine, the fractal properties of the fracture surface are studied. The results show that the fractured surface has anisotropic fractal characteristics.