2016年12月8日新疆呼图壁M_S6.2地震烈度分布初探  

Discussion on the Seismic Intensity of the Hutubi M_S6.2 Earthquake on December 8,2016

作　　者：罗炬[1] 陈建波[1] 常想德[1] 李帅[1] 孙静[1] 姚远[1] 

机构地区：[1]新疆维吾尔自治区地震局,乌鲁木齐830011

出　　处：《震灾防御技术》2017年第1期24-30,共7页Technology for Earthquake Disaster Prevention

摘　　要：根据182个烈度调查点的结果,结合余震序列分布、震源机制解和地震构造分析,编制呼图壁M_S6.2地震烈度图。极震区烈度为Ⅷ度,等震线长轴走向为EW向,发震构造为清水河子断裂。Based on the field investigation of 182 seismic hazard survey sites, combining with analysis of aftershock sequence, focal mechanism, and seismo-tectonic background, we produced the seismic intensity map of Hutubi Ms 6.2 earthquake. The seismic intensity of the magistoseismic area is VIH degree, with the orientation of long axis of isoseismic contour lines in east-west. The Qingshuihezi fault is considered as the seismogenic fault of Hutubi Ms 6.2 earthquake

关 键 词：新疆呼图壁 损失比 震害指数 地震烈度 

分 类 号：P315[天文地球—地震学]