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An inversion of site response and Lg attenuation using Lg waveform
作者姓名:朱新运  陈运泰
作者单位:Institute of Geophysics China Earthquake Administration,Institute of Geophysics China Earthquake Administration,Beijing 100081 ChinaEarthquake Administration of Zhejiang Province Hangzhou 310013 China,Beijing 100081 China School of Earth and Space Sciences Peking University Beijing 100875 China
基金项目:Zhejiang Province Science and Technology Plan (2007C33060),National Science and Technology Support Plan (2006BAC01B03-04-02).
摘    要:Based on spectral ratio method, a joint inversion method was used to obtain parameters of Lg wave attenuation and site response. The inversion method allows simple and direct (two-parameter) determination of Lg wave attenua- tion and site response from sparse spectral data, which are not affected by radiation pattern factor and different response of same instrument after geometrical spreading. The method was used successfully for estimating site re- sponse of stations of Zhejiang Seismic Network and measuring Lg wave attenuation. The study is based on 20 earth- quakes occurred in northeast of Taiwan with magnitude MS5.0~6.7 and 960 seismic wave records from 16 stations in Zhejiang area from 2002 to 2005. The parameters of site response and Lg attenuation were calculated with a fre- quency interval of 0.2 Hz in the range of 0.5 Hz to 10 Hz. Lg wave attenuation coefficient corresponding to U-D, E-W and N-S components are γ ( f )=0.00175 f 0.43485, γ ( f )=0.00145f 0.48467 and γ ( f )=0.0021f 0.41241, respectively. It is found that the site response is component-independent. It is also found that the site response of QIY station is significant above the frequency of 1.5 Hz, and that the site response of NIB station is low for most frequency

关 键 词:地震波  衰减参数  震源  现场反应
文章编号:1000-9116(2007)06-0605-12
收稿时间:2007-04-28
修稿时间:2007-08-31

An inversion of site response and Lg attenuation using Lg waveform
Zhu Xin-yun,and Chen Yun-tai.An inversion of site response and Lg attenuation using Lg waveform[J].Acta Seismologica Sinica(English Edition),2007,20(6):605-616.
Authors:Zhu Xin-yun  and Chen Yun-tai
Institution:(1) Institute of Geophysics, China Earthquake Administration, Beijing, 100081, China;(2) School of Earth and Space Sciences, Peking University, Beijing, 100875, China;(3) Earthquake Administration of Zhejiang Province, Hangzhou, 310013, China
Abstract:Based on spectral ratio method, a joint inversion method was used to obtain parameters of Lg wave attenuation and site response. The inversion method allows simple and direct (two-parameter) determination of Lg wave attenuation and site response from sparse spectral data, which are not affected by radiation pattern factor and different response of same instrument after geometrical spreading. The method was used successfully for estimating site response of stations of Zhejiang Seismic Network and measuring Lg wave attenuation. The study is based on 20 earthquakes occurred in northeast of Taiwan with magnitude M S5.0–6.7 and 960 seismic wave records from 16 stations in Zhejiang area from 2002 to 2005. The parameters of site response and Lg attenuation were calculated with a frequency interval of 0.2 Hz in the range of 0.5 Hz to 10 Hz. Lg wave attenuation coefficient corresponding to U-D, E-W and N-S components are γ(f)=0.00175f 0.43485, γ(f)=0.00145f 0.48467 and γ(f)=0.0021f 0.41241, respectively. It is found that the site response is component-independent. It is also found that the site response of QIY station is significant above the frequency of 1.5 Hz, and that the site response of NIB station is low for most frequency Foundation item: Zhejiang Province Science and Technology Plan (2007C33060) and National Science and Technology Support Plan (2006BAC01B03-04-02).
Keywords:Lg wave  site response  parameters of attenuation  joint inversion
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