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在对毛毛山断裂带断错微地貌划分对比的基础上详细分析了其位移分布特征。结果表明，毛毛山断裂的水平位移和垂直位移均具较明显的分组现象和可公度性特点。在空间分布上具明显的互补性，从东到西水平位移具累积滑动亏损特征，垂直位移则具累积滑动补偿性，这反映了沿断裂带活动性质与活动强度的差异性和非均匀性。位移累积滑动亏损直接反映了断裂在一定时段内的特征滑动行为，是进行分段的重要依据
Based on the comparison of the fault micro-topography in the Maomaoshan fault zone, the displacement distribution characteristics are analyzed in detail. The results show that both the horizontal and vertical displacements of the Maomaoshan fault have obvious grouping and commensurability characteristics. There is a clear complementarity in the spatial distribution. The horizontal slip from east to west has the characteristics of cumulative sliding loss, while the vertical displacement has cumulative slip compensation, which reflects the difference and inhomogeneity of the activity properties and activity intensity along the fault zone. The cumulative sliding loss of displacements directly reflects the characteristic sliding behavior of fractures in a certain period of time, which is an important basis for segmenting