针对鄂尔多斯周缘断陷盆地带，基于b值、Δb空间扫描和多参数（b、√E、n、a/b）组合计算结果，综合分析各段落的应力状态，进而判定它们的危险性。结果显示：整个周缘断陷带的年发生率、年释放率均整体下降，揭示出该区域2010年6月以来呈现出地震弱活动状态；b值较1970～2010年结果变化并不显著，内蒙古磴口-五原值得注意地区、同心-灵武值得注意地区、晋冀蒙交界危险区和侯马-运城值得注意地区4个区域仍处于匀速的应力积累状态；结合多参数组合揭示的应力状态和断裂习性，认为内蒙磴口-五原地区未来发震危险性最高，但近期发震的紧迫性不强，同心-灵武地区危险性有所增强，侯马-运城地区危险性持续，晋冀蒙交界地区危险性有所降低，其余段落近期复发强震的可能性不大。

Based on the calculation results of b-value,Δb spatially scanning and multiple-seismicity-parameter-value combinations(b, √E, n,a/b),we comprehensively analyze the stress state of basins around the Ordos block and then determine their risks. The results show that annually seismicity rate and annually strain-release-rate generally decrease in the fault depression belt around the Ordos block,revealing the weak seismicity of this region since June,2010. The difference of b-value between 1970~2018 and 1970~2010 is not obvious. The areas that are worthy of attention,including Dengkou-Wuyuan in Inner Mongolia,Tongxin-Lingwu,the junction zone of Shanxi-Hebei-Inner Mongolia and Houma-Yuncheng,remain constant stress accumulation state. Combined with the stress state reflected by multiple-seismicity-parameter-value combinations and fault habit,the probability of strong-earthquake is the highest in Dengkou-Wuyuan, Inner Mongolia,but the urgency of that in the near future is not strong. The risk of Tongxin-Lingwu area enhances a little. The risk of the Houma-Yuncheng area still continues. The risk of junction zone of Shanxi-Hebei-Inner Mongolia decreases a little. The probability of strong-earthquake on other sections is small in the near future.

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中国地震局地震预测研究所科研专项（2017IES010104、2017IES010105）、国家重点研发计划项目（2017YFC1500502-01）、山西省科技厅项目（201801D221044）和2019年度震情跟踪专项工作任务（2019010106）共同资助