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SPATIAL DISTRIBUTION FEATURES OF VELOCITY RESPONSES OF MW=8.0 EARTHQUAKE -CASE STUDY IN THE 2003 TOKACHI-OKI EARTHQUAKE-

机译:MW = 8.0地震波速度响应的空间分布特征-以2003年十日冈地震为例

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The 2003 Tokachi-oki earthquake, a large (Mw=8.0) inter-plate earthquake, is the first earthquake with a magnitude of 8 after the nation wide high-density strong-motion network was installed. We make the spatial distribution maps and attenuation relationships for velocity responses. The spatial distribution maps show different features depending on the period. The short period (T:natural period =0.1) sec map shows strong attenuation of the response at back-arc side of the volcanic front; this can be explained by the S-wave attenuation structure beneath the northern Japan. The long-period (T~10sec) maps and relations are in part controlled by the source effect and the deep subsurface structure.
机译:2003年的十胜冲木地震是板块间大地震(Mw = 8.0),是安装了全国性的高密度强运动网络后的第一场8级地震。我们为速度响应绘制了空间分布图和衰减关系。空间分布图根据时段显示不同的特征。短时间段(T:自然周期= 0.1)秒图显示了火山锋后弧侧响应的强烈衰减。这可以通过日本北部下方的S波衰减结构来解释。长周期(T〜10sec)的图和关系部分受源效应和深层地下结构控制。

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