Method for eliminating linear and non-linear interference wave by using filtering operation at deep layer domain
A technology of depth domain and interference wave, which is applied in the direction of seismic signal processing, etc., can solve the problems that the denoising method cannot completely separate the noise and the signal, the denoising effect cannot be achieved, and the statistical characteristics of frequency, apparent velocity, and propagation direction are difficult to distinguish, etc. , to achieve the effect of reducing spatial aliasing and eliminating incorrect continuation
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Embodiment 1
[0046] For the collected seismic shot data, the seismic data of a two-dimensional survey line is selected for depth-domain filtering processing. The basic situation of the data is as follows:
[0047] The data channel length is 4000ms, and the sampling interval is 4ms.
[0048] The survey line data includes 351 shots in total, and each shot has 800 traces.
[0049] 1) Firstly, data gain is performed, track equalization is performed on the data along the spatial x direction, and amplitude compensation is performed along the time direction, so that the data can be adapted to wave equation processing.
[0050] 2) Next, carry out two-dimensional Fourier forward transform and downward wave field continuation, and extend the shot set from the ground surface to the reference surface according to the formulas (4) and (5). The depth of the selected reference surface is 150m, which is divided into three layer, the thickness and speed of each layer are: 80m, 40m and 30m, 2000m / s, 2400m / ...
Embodiment 2
[0064] For the collected seismic shot data, the seismic data of one shot 3D survey line is selected for depth-domain filtering processing. The basic information of the data is as follows:
[0065] The data channel length is 6000ms, and the sampling interval is 2ms.
[0066] The data includes 8 survey lines, each with 192 traces.
[0067] Dx=40m, Dy=240m
[0068] 1) Firstly, data gain is performed, track equalization is performed on the data along the spatial x and y directions, and amplitude compensation is performed along the time direction, so that the data can be adapted to wave equation processing.
[0069] 2) Next, carry out the three-dimensional Fourier transform and extend the downward wave field. The shot set is extended from the ground surface to the reference plane according to the formulas (5) and (6). The depth of the selected reference plane is 150m, which is divided into three layers , the thickness and speed of each layer are: 80m, 40m and 20m, 2000m / s, 2400m / ...
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