孙继忠. 赤峰南部地区弱震活动是唐滦强震孕育和发生的窗口[J]. 华北地震科学, 1985, 3(4): 93-98.
引用本文: 孙继忠. 赤峰南部地区弱震活动是唐滦强震孕育和发生的窗口[J]. 华北地震科学, 1985, 3(4): 93-98.
Sun Jizhong. THE ACTIVITY OF WEAK SHOCKS IN THE SOUTH OF CHI FENG BEING THE WINDOW THAT STRONG EARTHQUAKES DEVELOP AND OCCUR IN TANG-LUAN[J]. North China Earthquake Sciences, 1985, 3(4): 93-98.
Citation: Sun Jizhong. THE ACTIVITY OF WEAK SHOCKS IN THE SOUTH OF CHI FENG BEING THE WINDOW THAT STRONG EARTHQUAKES DEVELOP AND OCCUR IN TANG-LUAN[J]. North China Earthquake Sciences, 1985, 3(4): 93-98.

赤峰南部地区弱震活动是唐滦强震孕育和发生的窗口

THE ACTIVITY OF WEAK SHOCKS IN THE SOUTH OF CHI FENG BEING THE WINDOW THAT STRONG EARTHQUAKES DEVELOP AND OCCUR IN TANG-LUAN

  • 摘要: 本文依据赤峰南部台网的实测资料,论述了该地小震活动与唐山大震及强余震的呼应关系。突出体现了小震活动的"窗口效应",并从小震活动规律探索其与地质构造的内在联系,试图为监测京津唐地区的大震提供依据和线索。

     

    Abstract: According to the data measured in the network in the south of Chi Feng, the co-rresponding relation between the activities of small shocks in the region and Tang Shan earthquake or its strong aftershocks has been discussed, and "the window effect" of small shock activities can be stressed in this paper.The author explores the inter-nal relation between the small shock activities and the geological structures, and tries to give some clue to monitor strong earthquakes in the Beijing-Tianjin-Tangshan region.

     

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