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Regional Variability Of Ground-Motion Of MS6.0-7.0 Earthquakes Between The North-South Seismic Zone In China And California Region

机译:M S 6.0-7.0地震地面运动的区域变异性和加利福尼亚州南北地震区之间的地震

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A large number of strong-motion recordings collected by the National Strong-Motion Observation Networks System during the MS6.0-7.0 earthquake occurred in the North-South Seismic Zone. We selected the strong-motion recordings with Joyner-Boore distance less than 400 km, and the ground motion prediction equation developed by Booer et al. (2014) to investigate the region variability of ground motion between the NSSZ and California region. The residual analysis was done to exhibit the regional variability of ground motion between both regions. The resultant between-events residuals suggested that the source effect in NSSZ region was stronger than that in California region. The adjustment coefficients of anelastic attenuation in NSSZ were larger compared with that in BSSA14 model, indicated that the NSSZ exhibited slower anelastic attenuation.
机译:在M个强大运动观测网络系统中收集的大量强运动记录 s 6.0-7.0地震发生在南北地震区。我们选择了joyner-boore距离小于400公里的强运动录制,并通过Booer等人开发的地面运动预测方程。 (2014)调查NSSZ和加利福尼亚地区地区地区运动的区域变异。完成残余分析以表现在两个地区之间的地面运动的区域变异。所产生的事件残差表明,NSSZ地区的源效应比加州地区强。与BSSA14模型相比,NSSZ中的Anelastic衰减的调整系数较大,表明NSSZ表现出较慢的Anelastic衰减。

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