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Seismic Hazard in the South Carolina Coastal Plain: 2002 Update of the USGS National Seismic Hazard Maps

机译:南卡罗来纳州沿海平原的地震危险:USGS国家地震危险性地图的2002年更新

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The damaging 1886 moment magnitude ~7 Charleston, South Carolina earthquake is indicative of the moderately likely earthquake activity along this portion of the Atlantic Coast. A recurrence of such an earthquake today would have serious consequences for the nation. The national seismic hazard maps produced by the U.S. Geological Survey (USGS) provide a picture of the levels of seismic hazard across the nation based on the best and most current scientific information. The USGS national maps were updated in 2002 and will become part of the International Codes in 2006. In the past decade, improvements have occurred in the scientific understanding of the nature and character of earthquake activity and expected ground motions in the central and eastern U.S. The paper summarizes the new knowledge of expected earthquake locations, magnitudes, recurrence, and ground-motion decay with distance. New estimates of peak ground acceleration and 0.2 s and 1.0 s spectral acceleration are compared with those displayed in the 1996 national maps. The 2002 maps show increased seismic hazard in much of the coastal plain of South Carolina, but a decrease in long period (1 s and greater) hazard by up to 20% at distances of over 50 km from the Charleston earthquake zone. Although the national maps do not account for the effects of local or regional sediments, deep coastal-plain sediments can significally alter expected ground shaking, particularly at long period motions where it can be 100% higher than the national maps.
机译:南卡罗来纳州查尔斯顿地震的1886矩矩震级为7,表明该大西洋海岸沿岸地震活动中等程度。今天这样的地震再次发生将对国家造成严重后果。美国地质调查局(USGS)制作的国家地震灾害图根据最佳和最新科学信息提供了全国地震灾害水平的图片。 USGS国家地图在2002年进行了更新,并将在2006年成为国际法规的一部分。在过去的十年中,对地震活动的性质和特征以及预期的美国中部和东部地震动的科学认识得到了改善。论文总结了关于预期地震位置,震级,复发和地震动随距离衰减的新知识。将峰值地面加速度以及0.2 s和1.0 s频谱加速度的新估计值与1996年国家地图中显示的估计值进行了比较。 2002年的地图显示,南卡罗来纳州沿海大部分地区的地震危险性增加,但距查尔斯顿地震带的距离超过50公里,长期(1秒或更长时间)的危险性降低了20%。尽管国家地图未考虑本地或区域沉积物的影响,但深海平原地区的沉积物会显着改变预期的地面震动,尤其是在长时间运动时,其可能会比国家地图高100%。

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