吕梦麟, 商宏宽. 晋冀鲁豫交界地区地震活动特征[J]. 华北地震科学, 1988, 6(4): 1-13.
引用本文: 吕梦麟, 商宏宽. 晋冀鲁豫交界地区地震活动特征[J]. 华北地震科学, 1988, 6(4): 1-13.
Lu Menglin, Shang Hongkuan. THE CHARACTERISTICS OF THE SEISMICITY AROUND THE JUNCTURE OF SHANXI, HEBEI, SHANDONG AND HENAN PROVINCES[J]. North China Earthquake Sciences, 1988, 6(4): 1-13.
Citation: Lu Menglin, Shang Hongkuan. THE CHARACTERISTICS OF THE SEISMICITY AROUND THE JUNCTURE OF SHANXI, HEBEI, SHANDONG AND HENAN PROVINCES[J]. North China Earthquake Sciences, 1988, 6(4): 1-13.

晋冀鲁豫交界地区地震活动特征

THE CHARACTERISTICS OF THE SEISMICITY AROUND THE JUNCTURE OF SHANXI, HEBEI, SHANDONG AND HENAN PROVINCES

  • 摘要: 本女通过对晋冀鲁豫交界地区历史的和近期的地震活动分析,阐述了该区地震活动特征。我们认为,一个乃至一组强震事件是大区域应力增强过程的反应。据此,对1830年磁县7.5级和1937年菏泽7.0级两次强震前的地震活动图象及其演变过程作了剖析,发现它们都经历了由大面积外围活动(有的出现地震条带)到范围缩小活动集中呈现活化状态的过程。文中还通过典型震例讨论了菏泽地震同唐山地震的呼应关系。有趣的是,这种呼应都是在华北地震活动处于较为平静的背景下出现的,这点值得今后进行地震活动趋势分折时注意。文中对该区今后应加强监测的危险部位提出了看法。

     

    Abstract: Basing on the analysis of the recent and histroical seismic activity anoand the junetre of Shanxi, Hebei, Shandong and Henan provinces, the characteristics of the seismicity in this area have been shown. It is suggested that a strong event or a groip of the strong shocks is the reflection of the stress increasing process. Based on this, seismic activity pattern and the developing process before 1830 Cixian 7.5 and 1937 heze 7.0 earthquakes have been analysised. It is obtained that the process from peripheral scismic activity (or seismic belt) in large scale to centralized activity of the cluster in small scale has been undergone. Then, the echo relation betwesa Heze earthquake and Tangshang earthquake has been discussed by typical shocks. It is interesting that the echo occurs in the seismically quiet period in North China. This situatioa should be noticed in the trend analysis of the funture seismicity. The areas that need to be strenghened in detection in recent have been suggested.

     

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