首页> 外文会议>World conference on earthquake engineering >ATTENUATION MODELS FOR RESPONSE SPECTRA DERIVED FROM JAPANESE STRONG-MOTION RECORDS ACCOUNTING FOR TECTONIC SOURCE TYPES
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ATTENUATION MODELS FOR RESPONSE SPECTRA DERIVED FROM JAPANESE STRONG-MOTION RECORDS ACCOUNTING FOR TECTONIC SOURCE TYPES

机译:响应光谱响应谱的衰减模型源于日本强运动记录核算构造源类型

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摘要

A spectral acceleration attenuation model for Japan is presented. It accounts for effects of tectonic source type and the faulting mechanisms for crustal earthquakes. Site class terms, instead of individual site correction terms, are used based on a recent study on site classification for strong motion recording stations in Japan. By using site class terms, source type effects are identified. For crustal and interface earthquakes, a simple form of attenuation model is able to capture the main strong motion characteristics and achieve unbiased estimates. For subduction slab events, a simple distance modification factor is employed to achieve plausible and unbiased prediction. Effects of source depth, tectonic source type, and faulting mechanisms for crustal earthquakes are significant.
机译:提出了日本光谱加速衰减模型。它占构造源类型的影响以及地壳地震的故障机制。站点类术语,而不是单个站点校正项,基于最近关于日本强运动录音站的现场分类研究。通过使用站点类术语,识别源类型效果。对于地壳和界面地震,简单的衰减模型形式能够捕获主要的强运动特性并实现无偏见的估计。对于俯冲板事件,采用简单的距离修改因子来实现可粘合和无偏的预测。地壳地震源深度,构造源型和断层机制的影响是显着的。

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