So the orthogonal seismic trace can reflect clearly some fuzzy and dim amplitude information in the record of the real seismic trace.
因此,正交地震道能突出反映实地震记录中某些模糊、朦胧的振幅信息。
But the normalized auto-correlation of real seismic acceleration record comprises an obviously random noise with amplitude value of 0.15 or so, that is so called super random content.
但是真实地震动的归一化自相关函数则有一较显著的随机噪声项,这个随机噪声的幅值为0。15左右,这就是本文中所说的超随机特性。
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