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Duration of strong ground motion during Northridge, California, earthquake of January 17, 1994

机译:1994年1月17日在加利福尼亚州北岭发生地震的强烈地面运动的持续时间

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摘要

Contours of spatial variations of the duration of strong earthquake ground motion during the 1994 Northridge, California earthquake are smooth over distances as large as tens of kilometers. Visual comparison of those contours with the depth of sediments and with vertical offsets of the basement rocks along the faults in the Los Angeles basin are in excellent qualitative agreement with the trends predicted by the previously published empirical scaling equations of strong-motion duration. It is argued that if the source-to-station distances were measured along the three-dimensional wave paths through the sedimentary wave-guides, rather than along straight lines as is common at present, the accuracy of empirical scaling equations could be improved significantly.
机译:在1994年加利福尼亚州北岭大地震中,强地震地震动持续时间的空间变化轮廓在长达数十公里的距离上都很平滑。这些轮廓与沉积物深度以及沿洛杉矶盆地断层的基底岩石垂直偏移的轮廓对比,与先前发表的强运动持续时间经验比例方程所预测的趋势具有极好的定性一致性。有人认为,如果沿沉积波导管的三维波路径而不是目前通常沿直线测量源到站距离,则可以显着提高经验比例方程的精度。

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