袁小沼. 邢台“震情窗口”的再分析[J]. 华北地震科学, 1991, 9(1): 67-73.
引用本文: 袁小沼. 邢台“震情窗口”的再分析[J]. 华北地震科学, 1991, 9(1): 67-73.
Yuan Xiaozhao. REANALYSIS FOR THE “SEISMIC WINDOW” OF XINGTAI[J]. North China Earthquake Sciences, 1991, 9(1): 67-73.
Citation: Yuan Xiaozhao. REANALYSIS FOR THE “SEISMIC WINDOW” OF XINGTAI[J]. North China Earthquake Sciences, 1991, 9(1): 67-73.

邢台“震情窗口”的再分析

REANALYSIS FOR THE “SEISMIC WINDOW” OF XINGTAI

  • 摘要: 在以往对邢台地震区的地震活动分析中,都将其作为"震情窗口"来观察华北地壳应力场的变化,预测这一地区的中强地震活动。本文用数理统计的方法,对邢台地震活动的异常进行了分析判断,提出了"震情窗口"除了能反映华北大范围的应力场变化或邻近邢台局部地点的应力变化外,还能反映邢台震区自身的应力集中现象。这是以往分析"震情窗口"时所忽视的。这对于发生过强烈地震并作为"震情窗口"的某些老震区的中强余震预报有一定的意义。

     

    Abstract: In the past analysis the seismic activity of Xingtai area is considered as a "seismie window" that is used to observe the crustal stress field of North China and predict the moderately strongearthquakes in this district.In this paper, mathematical statistic results are used to analyse and judge the seismic activity anomaly in Xingtai area and it is pointed out that the "seismic window" not only reflects the ehanging stress in North China or at some local sites near Xingtai, but also reflects the accumulating and eoncentratlng-stress in Xingtai "seismic window" itself.This was ignored in the analysis of the "seismic window" previously.It is significant for the prediction of the moderately strong aftershocks in some old seismic areas where great earthquakes occurred and which are regarded as "seismic windows".

     

/

返回文章
返回