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东日本大地震重力信号同震响应

Coseismic Response to Gravity Signals of the Great Earthquake in East Japan

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【作者】 王林松陈超梁青王秋革

【Author】 WANG Linsong1 CHEN Chao1 LIANG Qing1 WANG Qiuge1(1 Institute of Geophysics & Geomatics,China University of Geosciences(Wuhan),388 Lumo Road,Wuhan 430074,China)

【机构】 中国地质大学(武汉)地球物理与空间信息学院

【摘要】 对2011年3月11日日本本州东海岸附近海域Mw9.0级地震前后的观测重力资料进行了同震响应信号分析,给出了gPhone重力仪在大地震后的长周期地震面波和自由振荡的观测结果。震后12h数据经带通滤波后可以分辨出7个环绕地球传播的瑞雷波记录,在低频范围内(5mHz以下)检测到43个地球自由振荡基频振型及52个谐频振型,其分布与理论模型吻合较好。其中,在1mHz以下的低频段内观测到4个振型的谱峰分裂现象。

【Abstract】 We analyze the gravity data observed before and after March 11,2011 when the Mw9.0 earthquake occurred in the sea areas nearby the East coast of Honshu,Japan,with the method of co-seismic response signal analysis.We also provide the observations of long-period seismic surface waves and free oscillations recorded by gPhone gravimeter after the great earthquakes.Processed by band-pass filter,the data obtained within 12 hours after the earthquake can be recognized the records of 7 Rayleigh surface waves spreading around the Earth.In the low frequency domain(5 mHz or less),43 fundamental modes and at least 52 harmonic modes of Earth’s free oscillations can be detected,the distributions of which are in good agreement with the theoretical modes.Meanwhile,at the low frequencies less than 1 mHz,spectral splitting of 4 modes is observed.

【基金】 国家科技部国际科技合作专项资助项目(2010DFA24580);国家自然科学基金资助项目(40730317,40774060)
  • 【文献出处】 武汉大学学报(信息科学版) ,Geomatics and Information Science of Wuhan University , 编辑部邮箱 ,2012年11期
  • 【分类号】P315
  • 【被引频次】6
  • 【下载频次】93
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