Description: Test gabor deconvolution procedure
Seismic signal non-stationary signals, the wavelet is changing with time. Gabor deconvolution of seismic traces cut into several pieces Gabor in each sub-wave film is constant, it is possible to achieve a non-stationary signal to smooth signal conversion. Therefore, Gabor deconvolution is considered to be a high-resolution, true-amplitude reflection coefficient estimation method.
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Gabor反褶积
...........\abcd.mat
...........\bcd.mat
...........\Determine_Start_Stop_TraceNo.m
...........\Display_profile.m
...........\fgabor.m
...........\Find_seismic_header1.m
...........\gabordecon.asv
...........\gabordecon.m
...........\gaussian_upou.m
...........\gst_gabordecon_main.m
...........\igabor.m
...........\Line_subscript1.m
...........\test_gaborslice_未通.m
...........\test_single_trace.m
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