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首页> 外文期刊>Bulletin of the Seismological Society of America >Long-Period Ground-Motion Prediction Equations for Moment Magnitude Estimation of Large Earthquakes in Japan
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Long-Period Ground-Motion Prediction Equations for Moment Magnitude Estimation of Large Earthquakes in Japan

机译:日本大地震矩幅度估计的长周期地震动预测方程

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摘要

We developed long-period (5-30 s) ground-motion prediction equations (GMPEs) for peak ground velocities (PGVs) and peak ground displacements (PGDs) for crustal, interplate, and intraplate earthquakes. We used strong-motion data from KiK-net downhole stations located in layers with shear-wave velocities equal to or greater than 2000 m/s. The data set consisted of 20 earthquakes of 6 <= M-w <= 9.1 that occurred in and around Japan, including the 2011 Tohoku earthquake. Two-stage regression analyses were performed to derive the long-period GMPEs. We fitted the data with bilinear regression lines bending at M-w 7.5, although additional factors such as focal depth and earthquake type were found to enhance the fitting with the observed data. The developed equations indicated that long-period PGVs and PGDs are larger for crustal earthquakes than for interplate and intraplate earthquakes. The attenuation coefficients indicated that long-period PGVs and PGDs increase with increasing depth. We estimated the moment magnitude by fitting the observed PGVs and PGDs in the 5-30 s period range with the long-period GMPEs. We obtained estimates of the magnitudes of 23 earthquakes recorded by KiK-net downhole accelerometers, and the results were consistent with the moment magnitudes obtained from the Global Centroid Moment Tensor project. The described method was proven useful for estimating the moment magnitude of great earthquakes, offering the potential for rapid estimation of moment magnitude if information from the source area is available.
机译:我们针对地壳,板间和板内地震,针对峰值地面速度(PGV)和峰值地面位移(PGD)开发了长期(5-30 s)地震动预测方程(GMPE)。我们使用来自KiK-net井下站的强运动数据,该站位于剪切波速度等于或大于2000 m / s的层中。该数据集包括在日本及周边地区发生的20场6 <= M-w <= 9.1地震,包括2011年东北地震。进行了两阶段的回归分析,得出了长期的GMPE。尽管发现了其他因素(如震源深度和地震类型)可以增强与观测数据的拟合度,但我们使用弯曲于M-w 7.5的双线性回归线拟合了数据。发展的方程表明,地壳地震的长周期PGV和PGD比板间和板内地震大。衰减系数表明,长周期的PGV和PGD随着深度的增加而增加。我们通过在5-30 s的时间范围内将观测到的PGV和PGD与长周期GMPE拟合来估算矩量。我们获得了由KiK-net井下加速度计记录的23次地震震级的估计值,其结果与从全球质心矩张量项目获得的矩震级一致。实践证明,所描述的方法可用于估算大地震的矩震级,如果有震源区域的信息可用,则可提供快速估算矩震级的潜力。

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