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ＮＥ、ＮＷ 向断裂是青岛及其邻区两组重要的区域性断裂构造。通过野外地质和地貌观察，依据所测的地震活动和断裂活动的绝对年龄，认为青岛地区ＮＥ向断裂自晚更新—全新世以来处于相对稳定的阶段。并根据ＮＷ 向断裂对海岸线方向、海底地貌，特别是ＮＷ 向断裂对地震的控制作用，认为青岛及其邻区ＮＷ 向断裂是一组区域性活动断裂。鳌山卫—即墨微震带是ＮＷ 向断裂的现代活动性的表现。在地震监测工作中应加强对ＮＷ 向断裂活动性的监测与研究。
NE and NW trending faults are two important regional fault structures in Qingdao and its adjacent areas. Through field geology and geomorphology observation, based on the measured seismic activity and the absolute age of the fault activity, it is considered that the NE-trending fault in Qingdao area has been in a relatively stable phase since the late Pleistocene-Holocene. Based on the control of NW trending faults on the coastline, submarine geomorphology, especially the NW trending faults, NW trending faults in Qingdao and its adjacent areas are considered as a group of regional active faults. Aoshanwei - Jimo microseismic zone is NW active fracture performance of the show. Earthquake monitoring should be strengthened in the NW to the fault activity monitoring and research.