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The equation is valid for a constant velocity medium and is based on the wave number of the source and receiver.
Maximum amplitude measures the maximum positive or negative amplitude of a trace and potential low velocity medium within a time or depth window.
In a companion paper, Jakubowicz and Levin [2] showed that in a constant velocity medium the method is equivalent to the classical one-step 3D migration.
In numerical examples, effects of material composition, thermal loading, static axial loading, flow velocity, medium stiffness and shell geometry parameters on the free vibration characteristics are described.
The two-step approach originally introduced by Gibson et al. [1] is exact in a constant velocity medium explored with a zero-offset experiment, for example, with a monostatic radar system.
The standard method to migrate the diffractions observed in a medium where the velocity varies vertically consists of using the rms velocity function to extend the use of the equations derived for the constant velocity medium.
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The glenohumeral joint was scanned during active shoulder rotation at three angular velocities (low, medium and high velocities), with the arm by the side of the body by real-time cine MRI while recording with the help of a video camera.
(4)In this study, we used 4.0 km/s for the seismic velocity of medium β.
D represents the velocity of medium, (S_{0}) and (F_{0}) represent the input concentration of substrate and flocculating agent, respectively.
In experimental investigations, Peden et al. (1990) observed that pipe rotation has a significant effect on the minimum transport velocity in medium or highly viscous fluids and contributes to cuttings transport in small annulus or positive eccentricity.
The (rho V_{S}) is the S-wave impedance at the seismic station, where V s and ρ are, respectively, S-wave velocity and medium density at a seismic station.
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