摘要
本文采用作者提出的测定S波分裂时间延迟的方法,处理了大同—阳高地震、常熟地震和北京地区的中、小地震。结果表明,大同—阳高地区的地震活动性趋于正常,常熟地区应加强地震监测,北京地区的地震活动正常。
In this paper, a method of determing the time delay of shear wave splitting has been proposed by the author, with which the observed data fromDatong-Yanggao earthquake, Changshu earthquake and the moderate and smallevents in Beijing Area have been processed. The obtained results indicate that the seismic . activity features a normal tendency in Datong-Yanggao Area and in Beijing Area as well, whereas observations should be intensified in Changshu Area.
出处
《地震研究》
CSCD
北大核心
1991年第1期1-8,共8页
Journal of Seismological Research
基金
地震科学基金
关键词
地震
监测
S波
活动性
Shear wave splitting
Earthquake tendency
Datong-Yanggao earthquake
Changshu earthquake
