摘要
以汶川地震中的非发震断层安宁河断裂带周边西昌地区所获取的加速度记录为依据,研究了这些记录在峰值、频谱之间的差异,并通过这些地区的局部场地条件差异进行了初步解释。在此基础上通过数值模拟方法,利用基于显式有限元和局部透射人工边界的二维有限元模型对该地区的地面运动进行了模拟。数值试验结果表明:这些简单的理想化模型对这一地区地震动的本质特征进行重现,并对产生地面运动差异的机理进行合理解释。通过分析,初步揭示了由深部断层构造所控制的断陷盆地对地震动影响显著。
In this study,by analyzing the peak ground acceleration （PGA）and spectral character-istics of the earthquake acceleration records from the main shock of the Wenchuan earthquake, the difference of the ground motion at both sides of the Anninghe fault zone is discussed.By ana-lyzing the local site conditions at the observation stations,such as local site soil,topography,and tectonics,a preliminary explanation of the discrepancy is obtained,and the numerical solution of 2D model of this site derived by the explicit finite element combined with the local multi-trans-mitting artificial boundary method is used to interpret the mechanism causing the difference in the ground motion.The results of numerical calculations indicate that in spite of its simplicity,such an idealized model is also successful in reproducing many of the essential characteristics of ground motion and the mechanism causing the difference in ground motion within the fault zones of An-ninghe.The characteristics of the faulted basin under control of the Anninghe fault zone may be used to interpret observed seismic data obtained during the Wenchuan main shock and theoretical calculations of nearby fault responses in Xichang.
出处
《地震工程学报》
CSCD
北大核心
2014年第3期489-494,共6页
China Earthquake Engineering Journal
基金
中央高校基本科研业务费专项(ZY20110205
ZY20110206
ZY20120103)
国家自然科学基金(51208107
51308118)
关键词
断陷盆地
安宁河断裂
地震动记录
局部场地条件
数值模拟
faulted basin
Anninghe fault zone
ground motion
local site conditions
numerical simulation
