首页> 外文期刊>Bulletin of the Seismological Society of America >Basin Structure beneath the Santa Rosa Plain, Northern California: Implications for Damage Caused by the 1969 Santa Rosa and 1906 San Francisco Earthquakes
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Basin Structure beneath the Santa Rosa Plain, Northern California: Implications for Damage Caused by the 1969 Santa Rosa and 1906 San Francisco Earthquakes

机译:北加利福尼亚圣罗莎平原下的盆地结构:对1969年圣罗莎和1906年旧金山地震造成的破坏的影响

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摘要

Regional gravity data in the northern San Francisco Bay region reflect a complex basin configuration beneath the Santa Rosa plain that likely contributed to the significant damage to the city of Santa Rosa caused by the 1969 M 5.6, 5.7 Santa Rosa earthquakes and the 1906 M 7.9 San Francisco earthquake. Inversion of these data indicates that the Santa Rosa plain is underlain by two sedimentary basins about 2 km deep separated by the Trenton Ridge, a shallow west-northwest-striking bedrock ridge west of Santa Rosa. The city of Santa Rosa is situated above the 2- km-wide protruding northeast corner of the southern basin where damage from both the 1969 and 1906 earthquakes was concentrated. Ground-motion simulations of the 1969 and 1906 earthquakes, two events with opposing azimuths, using the gravity- defined basin surface, show enhanced ground motions along the northeastern edge of this corner, suggesting that basin-edge effects contributed to the concentration of shaking damage in this area in the past and may also contribute to strong shaking during future earthquakes.
机译:旧金山湾北部地区的区域重力数据 反映了圣罗莎 平原下的复杂盆地构造,这可能对 圣罗莎(Santa Rosa)市是由1969年的M 5.6、5.7级Santa 罗莎地震和1906年的M 7.9级旧金山地震引起的。这些数据的反演 表明圣罗莎平原位于 的两个沉积盆地之下,该沉积盆地的深约2公里,由 -Santa Rosa以西的西北基岩脊 。圣罗莎(Santa Rosa)市位于南部盆地 2公里宽的凸出东北角的上方,在此地区,1969年和1906年地震的破坏都集中在此。 1969年和1906年地震的地面运动模拟, 两个具有相反方位角的事件,使用重力定义的 盆地表面,沿东北方向显示出增强的地震动 该角的边缘,表明盆地边缘效应对 过去该区域的震荡破坏集中程度有所贡献,也可能对未来 地震时强烈震动。

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