The seismic amplitudes are usually strongest nearest the source and at early times. Consequently, the raw records usually show very weak or non-existent reflections at the far-offset traces. To display these important signals we gain the data in some fashion. This gain procedure can be a combination of several methods:
% % MATLAB 5.0 script for applying AGC to CSG traces in a CSG. % For each trace, the energy within a moving window of length % np is computed and the sample in the center part of this window % is divided by this energy. % % data(x,t) - input - nx x nt CSG matrix % np - input - length of AGC window % out1 - output- traces with AGC applied % [nx,nt]=size(data); inn=[fliplr(data(:,1:np)) data fliplr(data(:,nt-np:nt))]; inn=inn.^2; f=ones(np,1)/np; out=conv2(inn,f'); start=round(np+np/2);endd=start+nt-1; outt=out(:,start:endd); out1=data./(sqrt(outt)+.000001);