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胶东地区地壳S波衰减系数和台站场地响应的研究
引用本文:季爱东,李铂,张坤,赵金花,钟普浴.胶东地区地壳S波衰减系数和台站场地响应的研究[J].地震地磁观测与研究,2008,29(1):44-49.
作者姓名:季爱东  李铂  张坤  赵金花  钟普浴
作者单位:中国济南,250014,山东省地震局
基金项目:山东省地震局省局合同制项目
摘    要:根据山东数字地震台网7个地震台的118条波形资料,采用Atkinson方法(1992),研究了胶东地区的非弹性衰减系数;采用Moya方法(2000),研究了各台的场地响应。得到胶东地区非弹性衰减Q值随频率,的关系为Q(f)=249×f^0.596;得到的7个台站的场地响应均没有显示出明显的放大效应,这与胶东地区台站均处于岩石地基相符。

关 键 词:胶东地区  Q值  场地响应
文章编号:1003-3246(2008)01-0044-06
修稿时间:2007年8月20日

Study on S waves attenuation coefficient of crust and site response in Jiaodong region
Ji Aidong,Li Bo,Zhang Kun,Zhao Jinhua,Zhong Puyu.Study on S waves attenuation coefficient of crust and site response in Jiaodong region[J].Seismological and Geomagnetic Observation and Research,2008,29(1):44-49.
Authors:Ji Aidong  Li Bo  Zhang Kun  Zhao Jinhua  Zhong Puyu
Institution:(Earthquake Administration of Shandong Province, Jinan 250014, China)
Abstract:Bsed on 118 horizontal-component digital seismograms recorded at 7 seismic stations in Shandong Digital Seismograph Network, and with the methods of Atkinson (1992), the of inelastic attenuation coefficient in Jiaodong region is studied. By the methods of Moya (2000), the site response of each station is obtained. The frequency-dependent of inelastic attenuation coefficient Q is estimated as Q(f)=249×f^0.596 the site response of 7 seismic stations do not show significant Amplification, which is consistent with their basement on rock.
Keywords:Jiaodong region  Q value  site response
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