于新昌, 靳雅敏, 孙迎. 晋冀鲁豫交界地区的地震活动性估计[J]. 华北地震科学, 1985, 3(4): 52-60.
引用本文: 于新昌, 靳雅敏, 孙迎. 晋冀鲁豫交界地区的地震活动性估计[J]. 华北地震科学, 1985, 3(4): 52-60.
Yu Xinchang, Jin Yiamin, Sun Ying. THE STIMATION OF SEISMISITY IN THE JUCTURE OF SHANXI, HEBEI, SHANDONG AND HENAN PROVINCES[J]. North China Earthquake Sciences, 1985, 3(4): 52-60.
Citation: Yu Xinchang, Jin Yiamin, Sun Ying. THE STIMATION OF SEISMISITY IN THE JUCTURE OF SHANXI, HEBEI, SHANDONG AND HENAN PROVINCES[J]. North China Earthquake Sciences, 1985, 3(4): 52-60.

晋冀鲁豫交界地区的地震活动性估计

THE STIMATION OF SEISMISITY IN THE JUCTURE OF SHANXI, HEBEI, SHANDONG AND HENAN PROVINCES

  • 摘要: 本文利用晋冀鲁豫交界地区大量小地震的综合断层面解,对本区地震构造和地震活动关系进行了研究后提出:自1976年唐山大震后,该区小地震的综合断层面解的主压应力轴发生了转向,由近东西向转为近南北向,与华北地区强震发生的统一应力场不一致。对该区北西向的发震构造产生右旋滑动,而对应力积累起缓冲作用,从而使近年内,本区发生强震的可能性不大。但有可能存在中强地震活动。

     

    Abstract: Basing on the composite fault-plane solution of a lot of micro-earthquakes around the jucture of ShanXi, Hebei, Shandong and Henan provinces, it is suggested that, or the re-lationship between seismoteconic and seismicity, the direction of the principal pressure s-tress axis of the composite fault-plane solution hes turned into approximate the S-E from E-W direction since Tongshan earthquake, and isn't consistent with uniform stress field in North China, It effects right lateral slip for the northwestward earthquake fault and buffers stress accumulation.Theaeby, we concluded that it is almost impossible for strong shock to occur and possible for moderate strong earthquake.

     

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