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Data

It is difficult to understand the effects of $\epsilon$ and iterations when used for the inversion of real seismic data. Therefore, I chose to use a simple synthetic dataset provided to us by Bill Symes at The Rice Inversion Project (TRIP). It consists of one flat layer beneath a slow velocity lens. The velocity model can be seen in Figure [*]. The expected amplitude response from the flat reflector with regard to the offset ray parameter is constant.

 
vel
Figure 1
Velocity model for the TRIP synthetic. The lens is low velocity.
vel
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next up previous print clean
Next: Results Up: Effects of and niter Previous: Inversion operators
Stanford Exploration Project
7/8/2003