首页> 外文会议>World conference on earthquake engineering;WCEE >ATTENUATION MODELS FOR RESPONSE SPECTRA DERIVED FROMJAPANESE STRONG-MOTION RECORDS ACCOUNTING FORTECTONIC SOURCE TYPES
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ATTENUATION MODELS FOR RESPONSE SPECTRA DERIVED FROMJAPANESE STRONG-MOTION RECORDS ACCOUNTING FORTECTONIC SOURCE TYPES

机译:日语强运动记录对应构造源类型的响应谱的衰减模型

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A spectral acceleration attenuation model for Japan is presented. It accounts for effects of tectonic sourcetype and the faulting mechanisms for crustal earthquakes. Site class terms, instead of individual sitecorrection terms, are used based on a recent study on site classification for strong motion recordingstations in Japan. By using site class terms, source type effects are identified. For crustal and interfaceearthquakes, a simple form of attenuation model is able to capture the main strong motion characteristicsand achieve unbiased estimates. For subduction slab events, a simple distance modification factor isemployed to achieve plausible and unbiased prediction. Effects of source depth, tectonic source type, andfaulting mechanisms for crustal earthquakes are significant.
机译:提出了日本的频谱加速度衰减模型。它解释了构造源类型的影响和地壳地震的断裂机制。基于最近对日本强运动记录台的站点分类研究,使用站点类别术语代替了单个站点校正术语。通过使用站点类术语,可以识别源类型影响。对于地壳和界面地震,一种简单形式的衰减模型能够捕获主要的强运动特征并获得无偏估计。对于俯冲平板事件,采用简单的距离修正因子来实现合理且无偏的预测。震源深度,构造震源类型和断层断裂机制对地壳地震的影响很大。

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