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Fault zone amplified waves as a possible seismic hazard along the Calaveras fault in central California

机译:断层带放大波可能是加州中部卡拉维拉斯断层的潜在地震危险

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摘要

The Calaveras fault lies within a lo rv velocity zone (LVZ) 1-2 km wide near Gilroy, California. Accelcro- zone (LVZ) 1-2 km wide near Gilroy, California. Accelcrographs G06, located in the LVZ 1.2 km from the Calaveras fault, and G07, 4 km from G06, recorded both the M 6.2 1984 Morgan Hill and the M 6.9 1989 Loma Prieta earthquakes. Comparison of the ground motions shows that a large 0.6-1.0 Hz velocity pulse observed at G06 during the Morgan Hill event may be amplified by focussing caused by the LVZ. Such amplified waves might be a mappable seismic hazard, and the zone of increased hazard can extend as much as 1.2 km from the surface trace of the fault. Finite-difference simulations of ground motions in a simplified LVZ model show a zone of amplified motion similar to the observations. [References: 13]
机译:卡拉维拉斯断层位于加利福尼亚吉尔罗伊附近1-2公里宽的速度区(LVZ)内。加利福尼亚吉尔罗伊附近的加速区(LVZ)宽1-2公里。 Accelcrographs G06位于距卡拉维拉斯断层1.2公里的LVZ地带,而G07离G06则4公里,记录了1984年6.2摩根山和1989年6.9洛马普里埃塔M地震。地面运动的比较表明,在Morgan Hill事件期间在G06观测到的0.6-1.0 Hz大的速度脉冲可能会因LVZ引起的聚焦而放大。此类放大波可能是可映射的地震危险,危险增加的区域可能距断层表面迹线多达1.2 km。在简化的LVZ模型中,地面运动的有限差分模拟显示了类似于观测结果的放大运动区域。 [参考:13]

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