Seismic reflection data are always contaminated with short- and long-duration environmental and coherent noise. Long-duration coherent noise usually has a pseudo-sinusoidal wave form. Vehicles and power lines are major sources of environmental pseudo-sinusoidal noise. There are several methods for the attenuation of this noise, each with its own advantages and limitations. In this approach, this noise was considered as the reference noise, assuming that the noise is sinusoidal with phase and amplitude varying with time. To obtain the amplitude of the reference noise, an envelope of absolute data is depicted. To calculate its phase, firstly the frequency content of this noise versus time was calculated using a novel time?frequency transform that we named the weighted Fourier transform. Then, by integrating of calculated frequency, the phase was obtained. In the next step, to construct a trace containing noise, a filter was designed and convolved with reference noise. Then by subtraction of the constructed trace containing noise from the input seismic trace, the observed noise was highly attenuated.
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