文件名称:GaborDecon_test
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测试gabor反褶程序
地震信号是非平稳信号,其子波是随时间变化的。Gabor反褶积技术地震道切成若干个Gabor 片,在每一片中子波是不变的,因此可以实现将非平稳信号向平稳信号的转换。因此,Gabor反褶积被认为是高分辨率、真振幅反射系数的估计方法。-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.
地震信号是非平稳信号,其子波是随时间变化的。Gabor反褶积技术地震道切成若干个Gabor 片,在每一片中子波是不变的,因此可以实现将非平稳信号向平稳信号的转换。因此,Gabor反褶积被认为是高分辨率、真振幅反射系数的估计方法。-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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下载文件列表
Gabor反褶积/
Gabor反褶积/abcd.mat
Gabor反褶积/bcd.mat
Gabor反褶积/Determine_Start_Stop_TraceNo.m
Gabor反褶积/Display_profile.m
Gabor反褶积/fgabor.m
Gabor反褶积/Find_seismic_header1.m
Gabor反褶积/gabordecon.asv
Gabor反褶积/gabordecon.m
Gabor反褶积/gaussian_upou.m
Gabor反褶积/gst_gabordecon_main.m
Gabor反褶积/igabor.m
Gabor反褶积/Line_subscript1.m
Gabor反褶积/test_gaborslice_未通.m
Gabor反褶积/test_single_trace.m
Gabor反褶积/abcd.mat
Gabor反褶积/bcd.mat
Gabor反褶积/Determine_Start_Stop_TraceNo.m
Gabor反褶积/Display_profile.m
Gabor反褶积/fgabor.m
Gabor反褶积/Find_seismic_header1.m
Gabor反褶积/gabordecon.asv
Gabor反褶积/gabordecon.m
Gabor反褶积/gaussian_upou.m
Gabor反褶积/gst_gabordecon_main.m
Gabor反褶积/igabor.m
Gabor反褶积/Line_subscript1.m
Gabor反褶积/test_gaborslice_未通.m
Gabor反褶积/test_single_trace.m
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