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2004年9月17日阳江4.9级地震概述
引用本文:叶秀薇,杨马陵,叶东华,康英,秦乃刚,刘特培,万永芳,廖桂金,华卫.2004年9月17日阳江4.9级地震概述[J].华南地震,2005,25(3):69-77.
作者姓名:叶秀薇  杨马陵  叶东华  康英  秦乃刚  刘特培  万永芳  廖桂金  华卫
作者单位:广东省地震局,广东,广州,510070
摘    要:2004年9月17日广东阳江发生了4.9级地震,从地震序列、震中位置及等震线分布判断本次4.9级地震仍属1969年阳江6.4级地震"老"震区的晚期地震活动,与该区已发生的4~5级地震序列活动类似,具有前期余震频度、强度衰减快的特点.宏观调查及震源机制证实平冈断裂是此次4.9级地震的主要控震和发震构造.震前曾出现了一定数量的前兆异常,但地震学异常不显著,震前中小地震活动未出现异常活跃或异常平静.

关 键 词:震源机制  地震活动性  前兆异常  阳江地震
文章编号:1001-8668(2005)03-0069-09
收稿时间:2005-07-15
修稿时间:2005年7月15日

Summary of the M4.9 earthquake occurred in Yangjiang on September 17, 2004
YE Xiu-wei,YANGMa-ling,YE Dong-hua,KANG Ying,QIN Nai-gang,LIU Te-pei,WAN Yong-fang,LIAO Gui-jin,HUA Wei.Summary of the M4.9 earthquake occurred in Yangjiang on September 17, 2004[J].South China Journal of Seismology,2005,25(3):69-77.
Authors:YE Xiu-wei  YANGMa-ling  YE Dong-hua  KANG Ying  QIN Nai-gang  LIU Te-pei  WAN Yong-fang  LIAO Gui-jin  HUA Wei
Institution:Earthquake A dministration of Guangdong Province, Guangzhou 510070 , China
Abstract:On September 17, 2004, an M4.9 earthquake occurred in Yangjiang, Guangdong Province. We estimate that this earthquake is a continued seismicity of the M6.4 earthquake occurred in Yangjiang in1969, based on the analysis of the seismic sequence, the location of the epicenter and the isoseismal map. The aftershock frequency and intensity of this M4.9 earthquake attenuated very soon. The macro-investigation and focal mechanism approve that Ping-gang fault is the primary seismogenic structure. Some precursor anomalies had appeared before the earthquake happened, but few seismological anomalies emerged and the moderate and small earthquakes before the main shock were not anomalously active or anomalously quiet.
Keywords:Focal mechanism  Seismicity  Precursor anomaly  Yangjiang earthquake
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