CAJ | 학술논문

从郯庐断裂（沈阳-渤海段）地质构造和地球物理场特征出发，借助历史中强震复发周期和地震时空分布特征，对该区强震的危险性做了初步分析。结果表明该区6级和7级地震复发周期分别为18年和95年。目前郯庐断裂沈阳-渤海段接近6．5级地震的复发时段，值得注意地区为NNE向郯庐断裂与NW（或NNW）向断裂的交汇部位以及4级地震活动集中区附近。
종담려단렬（침양-발해단）지질구조화지구물리장특정출발，차조역사중강진복발주기화지진시공분포특정，대해구강진적위험성주료초보분석。결과표명해구6급화7급지진복발주기분별위18년화95년。목전담려단렬침양-발해단접근6．5급지진적복발시단，치득주의지구위NNE향담려단렬여NW（혹NNW）향단렬적교회부위이급4급지진활동집중구부근。
Based on the geological structure and geophysical field features of Tan-Lu fault (Shenyang- Bohai section) , a preliminary analysis about strong earthquake risk in the area is made by using the recurrence interval of history medium-strong earthquakes and the characteristics of temporal and spatial distribution. The results showed that M6.0 and M7.0 earthquakes'recurrence interval in this area was 18 years and 95 years respectively. Now it is close to M6.5 earthquake recurrence period of Tan-Lu fault (Shenyang-Bohai section) .The intersections of NNE direction of and NW direction (or NNW direction) of Tan-Lu fault fractures and ME4.0 seismicity concentration areas should be particularly concerned.