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作 者:陈绍明[1] 解用明[1] 赵英萍[1] 谢美娟[1] 将邦本[2] 刘绮亮[3]
机构地区:[1]河北省地震局,中国石家庄050021 [2]北京大学,中国北京100871 [3]国家地震局地球物理研究所,中国北京100081
出 处:《地震》1997年第1期14-24,共11页Earthquake
摘 要:利用华北地区近20a来的资料,对地磁日变低点位移与地震的关系进行了统计研究,并在此基础上建立了地震的短临预报指标。统计结果表明,低点位移分界线的分布与震中的分布有较好的一致性,两者均为网络状分布。还获得了一些可以区分震中区异常和非震中区异常的信息,并且初步确定了提取这个信息量的方法。This paper statistically studied the relationship between seismicity and thelow-point displacement of the daily geomagnetic variation by using the data of the lasttwo decades in North China, based on which the index of the short- term and imminentearthquake prediction was established. The statistical result shows that the distributionof the low-point disp1acement boundary is quite coincident with the epicenter distribu-tion, both distributed in netted pattern. The further research on the feature of theIow-point displacement also obtained some information, which can discriminate theanomaly of the epicentral region from that of the non-epicentral regions. The tech-niques for extracting this information were preliminarily determined. It is practically sig-nificant to diminish the range of the prediction region.
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