节点文献

局部地质条件对强地面运动影响的剪切波模拟

SH-WAVE MODELING OF INFLUENCE OF LOCAl GEOLOGICAL CONDITION ON STRONG GROUND MOTION

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 孙若昧F.VaccariG.F.Panza

【Author】 SUN RUO-MEI; F.VACCARI; G.F.PANZA(l Institute of Geology and Geophylsics, Chinese Academy of Sciences, Beijing 100101, China2 Dipartimento di Scienze della Terra, Universita’ degli Studi di Trieste, Trieste 34127,Italy.3 International Center for Theoretic

【机构】 中国科学院地质与地球物理研究所!北京100101DipartimentodiScienzedella.Terra.Universita’degliStudidiTrieste!31000ItalyCNR-GNDTGruppo Nazionale per?

【摘要】 采用多阶振型和有限差分联立的混合法,依据北京西集一郎府地区的地质条件,模拟了1976年唐山地震所引起的该区的剪切波运动;计算了工程上常用的峰值加速度和总能量.在夏垫断裂两侧的最大振幅和总能量的差异分别为200%和700%,研究结果可以解释唐山地震时西集一郎府一带所观测到的异常烈度.

【Abstract】 In this paper a hybrid method, based on mode summation and finitedifferences, is used to simulate the ground inchon of SH wave in the Xiji-Langfuarea of Beijing induced by the 1976 Tangshan earthquake. We eshmate the maximumacceleration amplitude and total energy of ground inchon for engineering purposes. Onthe two sides of the Xiadian fault the maximum acceleration amplitude and totalenergy can vary by afactor of 200% and 700% respectively. Our results can explainthe observed anomalous intensity in the Xiji-Langfu area induced by the 1976Tangshan earthquake.

  • 【文献出处】 地球物理学报 ,Chinese Journal of Geophysics , 编辑部邮箱 ,2000年01期
  • 【分类号】P315
  • 【被引频次】9
  • 【下载频次】92
节点文献中: 

本文链接的文献网络图示:

本文的引文网络