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首页> 外文期刊>Seismological research letters >Update of Urban Seismic-Hazard Maps for Memphis and Shelby County, Tennessee: Geology and V_S Observations
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Update of Urban Seismic-Hazard Maps for Memphis and Shelby County, Tennessee: Geology and V_S Observations

机译:田纳西州孟菲斯和谢尔比县的城市地震危险性地图的更新:地质和V_S观测

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摘要

In 2004, Memphis urban seismic-hazard maps were completed for a six-quadrangle area centered on Memphis and southern Shelby County (Cramer et al., 2004, 2006, 2008). Both probabilistic and scenario seismic and liquefaction hazard maps were generated for the six-quadrangle study area. These urban seismic-hazard maps, particularly the liquefaction hazard maps, have been used by consultants and public agencies to address seismic-hazard mitigation in the Memphis area. Memphis has the second highest annualized expected loss (AEL, expected losses to building inventory times frequency of occurrence) and the highest seismic hazard and AEL ratio (normalized by the building inventory exposed to loss) in the central and eastern United States (Petersen et al., 2008; Federal Emergency Management Agency [FEMA], 2008). Additionally, the U.S. Geological Survey (USGS) National Seismic Hazard Model (NSHM) has been updated since the first Memphis urban seismic- hazard maps were completed in 2004 with significant changes in the NewMadrid source model (number and weighting on alternative fault-rupture locations and distinctions in occurrence rates on the north, central, and south segments) and attenuation relations (updated and added relations showing on average lower ground motions; Petersen et al., 2008) that influence Memphis hazard.
机译:2004年,以孟菲斯和南部谢尔比县为中心的六个四角形区域完成了孟菲斯城市地震灾害图(Cramer等人,2004、2006、2008)。为六个四边形研究区域生成了概率图和情景地震和液化危害图。顾问和公共机构已使用这些城市地震危险性地图,尤其是液化危险性地图来解决孟菲斯地区的地震危险性减轻问题。孟菲斯在美国中部和东部的年度预期损失(AEL,建筑物清单的预期损失乘以发生频率)第二高,地震危险性和AEL比率(以遭受损失的建筑物清单标准化)最高(Petersen等人) (2008年;联邦紧急事务管理局[FEMA],2008年)。此外,自2004年完成第一张孟菲斯城市地震灾害图以来,美国地质调查局(USGS)的国家地震灾害模型(NSHM)进行了更新,其中NewMadrid震源模型发生了重大变化(替代断层破裂位置的数量和权重)以及北部,中部和南部分段的发生率的区别)和影响孟菲斯灾害的衰减关系(更新的和增加的关系显示平均较低的地面运动; Petersen等,2008)。

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