摘要
本文根据对山西隆起区断陷地震带内各区地震(M≥5)活动性的定量分析和历史地震震中迁移规律的对比,得出了该地震带内下次大震发生在渭河盆地断陷带的可能性较大的结论。并对渭河盆地未来大震的震级作出了估计。
Based on the quantitative analysis of seismic (M≥5) activity in each region of concave seismic belt of the uplift area in Shaanxi Province and the comparison of seismic central removal laws in history, it is eoneuluded that there might be a strong earthquake shock in Weihe river basin of this seismic belt. Besides, seismie class in this basin in the future is estimated.
出处
《陕西师大学报（自然科学版）》
CSCD
1989年第3期63-66,共4页
Journal of Shaanxi Normal University(Natural Science Edition)
