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A possible UL Fseismice lectro-magnetic emission
引用本文:李兴才,曹惠馨,俞铁宏. A possible UL Fseismice lectro-magnetic emission[J]. 地震学报(英文版), 1995, 8(3): 463-471. DOI: 10.1007/BF02650575
作者姓名:李兴才  曹惠馨  俞铁宏
作者单位:Xing-Cai LI;Hui-Xin CAO;Tie-Hong YU; and Zhi-YongCHEN; (Institute of Geophysics,State Seismological Bureau,Beijing 100081,China)(Seismological Bureau of Langfang,Langfang 102800,Hebei Province,China)
摘    要:ApossibleULFseismicelectro-magneticemissionXing-CaiLI;(李兴才)Hui-XinCAO;(曹惠馨)Tie-HongYU;(俞铁宏)andZhi-YongCHEN;(@2陈智勇)(Instituteo...

收稿时间:1994-02-23
修稿时间:1994-08-29

A possible ULF seismic electro-magnetic emission
Xing-Cai Li, Hui-Xin Cao, Tie-Hong Yu and Zhi-Yong Chen. A possible ULF seismic electro-magnetic emission[J]. Acta Seismologica Sinica(English Edition), 1995, 8(3): 463-471. DOI: 10.1007/BF02650575
Authors:Xing-Cai Li   Hui-Xin Cao   Tie-Hong Yu  Zhi-Yong Chen
Affiliation:(1) Institute of Geophysics, State Seismological Bureau, 100081 Beijing, China;(2) Seismological Bureau of Langfang, 102800 Langfang, Hebei Province, China
Abstract:A possible electro-magnetic emission (EME) associated with earthquakes are presented in the paper through analysis of the anomaly EME in ultra-low frequency range (ULF) observed at some sites before two earthquakes near Beijing and the comparison with similar signals observed prior to the 1988 Armenia and 1989 Loma Prieta earthquakes. The anomaly features are as follows: (1) the anomalous disturbances occur discontinuously several days before earthquakes and signal frequencies are higher remarkably than geomagnetic pulsation and magnetic disturbances during magnetic storms in ULF band and at least not lower than 1 Hz; (2) similar signals are observed by similar observation systems at same site for the same earthquake; (3) the anomaly occurrence times and frequencies at sites near the epicenter are earlier and higher respectively than that at farther sites; (4) the signal energy distribution in different frequency ranges may not be the same and the signal magnitudes may be related to earthquake magnitudes and greater earthquake may emit stronger EME signals; (5) there may be a seismic magnitude threshold for observable ULF EME anomalies and if smaller earthquakes possess of EME signals also, they may not be observed by the present observation system. Contribution No. 95A0062, Institute of Geophysics, SSB, China. Funded by the “8th Five-Year Plan” of State Seismological Bureau, contract code 85-907-03-02-05.
Keywords:electro-magnetic emission   short-impeding Prediction   ULF frequency band
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