论文部分内容阅读
本程序是在水平迭加记录上实现的。根据地震记录同相轴相干性的程度而进行加权,目的是突出规则波,削弱无规则的随机干扰。假设地震剖面A_i(t)是多维平稳随机过程,它由有效信号S(t)和随机干扰n_i(t)组成
This procedure is superimposed on the record level achieved. Weighted according to the degree of coherence of seismic events, the purpose is to emphasize the regular wave and weaken the irregular random disturbance. Assuming that the seismic section A_i (t) is a multidimensional stationary stochastic process consisting of a valid signal S (t) and a random disturbance n_i (t)