ISSN 1004-4140
CN 11-3017/P
S.法斯特霍夫, 郭履灿. 论震波频谱图—地震波的三维显示(英文)[J]. CT理论与应用研究, 2001, 10(3): 47-51.
引用本文: S.法斯特霍夫, 郭履灿. 论震波频谱图—地震波的三维显示(英文)[J]. CT理论与应用研究, 2001, 10(3): 47-51.
Stefan Fasitehuofu, Guo Lücan. On Spectral Seismograms-3D Display of Seismogram[J]. CT Theory and Applications, 2001, 10(3): 47-51.
Citation: Stefan Fasitehuofu, Guo Lücan. On Spectral Seismograms-3D Display of Seismogram[J]. CT Theory and Applications, 2001, 10(3): 47-51.

论震波频谱图—地震波的三维显示(英文)

On Spectral Seismograms-3D Display of Seismogram

  • 摘要: 震波频谱图,又名“震波凸形图(seismic topography)”是S.J.Duda关于谱震级概念的发展。对应于宽频带地震图相应于每一道带通频率fm来折算的瞬时振幅所组成的面(为二维包络面),沿着时间轴作出剖面,例如0.3赫芝的带中频率相匹配的带通滤波器所输出的包络线。而三维可视化技术则允许快速估算其相应振幅的分布,要能判明其高峰位置的相应分布,则不太容易,因此我们就将其剖面投影在二维的分布图上。为了辨识震波强度的分布,将此图配上相应的颜色,及其前置的颜色标尺,与其振幅值相对应。图中的等值线有助于识别图中的峰和谷并与高或低强度相对应。这种对宽频记录时间一频率分布的表达方式,用颜色和等值线来表示振幅值,我们称它为“频谱震波图”。可转化为三维图形,其中每一条线代表由相应带中频率fm计算得的包络线,用灰度表示等值线,估算震波强度或振幅的二维分布,又称为“震波凸形图”,它反映了在地震台记录的信号能量随频率和时间的分布,从而看出其最大强度所对应的频率范围。震波频谱图允许对随时间而变化的频谱分量在时间和强度的定位方面有较好的分辨率。在中国及邻近地区已试用该方法,说明有助于识别地震系列的特征。

     

    Abstract: This paper describe the spectral seismogram(seismic topography) had developed the concept of spectral magnitude which was introduced by S.J. Duda, the calibration functions for broad-band digital recordings of P-waves. The method of spectral seismograms, which was developed by Stefan Fasthoff and Duda to analyse Strong shock in and near China in recent years. This method had been used to classify seismic sequence types by its color feature: red-quake with lower frequency in P or S-wave group, and blue-quake which contained with more larger frequency elements in P or S-wave group by the filter of digital seismic records.

     

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