Oblique Disturbance Rejection Method Based on Linear Event Iterative Tracking Attenuation
A linear interference and event technology, applied in seismology, instruments, measuring devices, etc., can solve problems such as misleading seismic geological interpretation, loss of effective reflection signals from far offset traces, strong amplitude spatial aliasing, etc., to reduce damage Possibility of valid signal, clear efficiency advantage, effect of avoiding spatial aliasing
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[0029] In field seismic exploration, seismic waves are excited by sources such as explosives, air guns, or electric sparks, and seismic signals are received by geophones to obtain seismic records containing linear interference waves such as direct waves, refracted waves, or surface waves.
[0030] Sea area A is a hard seabed area, the seabed is relatively flat, and the water depth changes gently between 90 meters and 110 meters. Selected survey line X 1 It is about 45 kilometers long and uses 480 channels to receive. The shot interval and track interval are 50 meters and 12.5 meters respectively, the minimum offset distance is 170 meters, and the data sampling interval and record length are 0.004 seconds and 4.5 seconds respectively. Since the seabed is a strong reflection interface, the corresponding seismic data has strong direct wave and refracted wave interference, which seriously affects the subsequent processing effects of random noise attenuation, ghost wave elimination...
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