用地脉动研究银川沉积地层的地震波放大特性
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
根据银川盆地不同厚度覆盖层上的三分向( 东西、南北和垂直) 地脉动测量数据,绘制出水平向振幅谱与垂直向振幅谱的比值曲线.结果表明,谱比曲线上最大峰值处的频率大小显著地反映了覆盖层的薄厚.通过银川市部分房屋自振频率的对比分析认为,该部分房屋在未来地震中将遭受严重破坏.
Based on tri component measurement of microtremor on different thickness sediment layers in Yinchuan basin,the curves of ratio of horizontal spectrum to vertical spectrum were drawn.These curves show that the frequency value corresponding to maximum peak obviously reflect the sediment layers' thickness. Comparing the frequency value with predominant frequency of some buildings in Yinchuan,it can be concluded that these buildings would be seriously damaged by future earthquakes.
引文
[1] 李杰,等.地震工程学导论[ M].北京:地震出版社,1992 .
    [2] 孟广魁,等.银川平原地震区划研究[ M] .银川:宁夏人民出版社,1994 .
    [3] 刘惠珊,等.地震区的场地与地基基础[ M] .北京:中国建筑工业出版社,1994 .
    [4] 建设部抗震办公室.建筑抗震设计规范(GBJ11 - 89)统一培训教材[M] .北京:地震出版社,1990 .
    [5] Fischer K M,etal.Sedimentinduced amplificationinthe Northeastern United State:acasestudyin Providence,RhodeIsland[J] .Bull.Seism .Soc.Am .,1995 ,85 :1388~1397.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心