摘要
为满足数字化时代应急处置的新要求,基于随机有限断层法的发展,利用青海门源地区地下三维速度结构的模型和v S30数据,通过逐步迭代射线追踪法、格林函数位移解析相位谱和有限断层法的联合计算,以青海门源6.9级地震为例,获得具有地表土层放大效应的强地震动模拟数据,进而绘制出研究区内PGA和烈度分布模拟图;并与实际台站记录的PGA和实地调查烈度结果相比,其烈度区划范围基本一致,同时也验证此联合计算方法可用于未来地震灾害的快速评估,并为灾后应急救援提供参考。
To address the modern requirements of emergency response efforts in the digital age,we developed an approach based on the stochastic finite fault method.Specifically,utilizing an underground three-dimensional velocity structure model and v S30 data from the Menyuan region of the Qinghai Province,we applied the step-by-step iterative ray-tracing method,phase spectrum of Green's function displacement analytical solution,and finite fault method to record strong ground motion simulation data incorporating ground surface amplification effects.Furthermore,considering the Menyuan M 6.9 earthquake that struck the Qinghai Province on January 8,2022,we created simulation maps depicting the peak ground acceleration(PGA)and intensity distributions within the study area.Subsequently,comparing the simulated results with actual PGA records from monitoring stations and field survey intensity data revealed consistent intensity zonation scopes.Moreover,these results validated the utility of the proposed method for rapid assessments of future earthquake disasters,offering valuable insights for postdisaster emergency rescue efforts.
作者
师涵博
张元生
SHI Hanbo;ZHANG Yuansheng(Lanzhou Institute of Seismology,CEA,Lanzhou 730000,Gansu,China)
出处
《地震工程学报》
CSCD
北大核心
2024年第3期680-691,共12页
China Earthquake Engineering Journal
基金
甘肃省科技重大专项“甘肃重点地区地震预测预警新方法与新技术”(21ZD4FA011)。
关键词
门源地震
强地震动模拟
有限断层法
逐步迭代射线追踪法
Menyuan earthquake
strong ground motion simulation
finite fault method
step-by-step iterative ray-tracing method