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This synthetic model is essentially composed of two constant velocity layers
with a transient zone between the two layers. The geometrical size of this
model is the same as last one. The velocity of upper layer is
2000m/s and that of lower one 3000m/s. The interface will make the
Runge-Kutta algorithm fail if the model is not smoothed reasonably. We apply
a triangle smoothing filter to the model along x, y, z axis. The result
is shown in Figure 4.
model2-smooth
Figure 4 Left: The sharp interface makes the Runge-Kutta algorithm fail. The rays propagate in random directions when passing through the interface. Some of them are even reflected back to the upper layer. Right: The interface has been smoothed by the triangle smoothing filter. The rays' propagating directions follow Snell's law. All the rays pass through the transition zone and enter the lower layer.
Next: EAEG/SEG saltdome model
Up: RESULTS AND DISCUSSION
Previous: Synthetic model (linear velocity)
Stanford Exploration Project
11/11/1997