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Complex subsurface distorts multiples and make their identification difficult in the image space.
We can either compute an approximate multiple model with an image space version of SRME or, better,
compute full 3D angle gathers in order to exploit the different characteristics of the residual
moveout of the multiples and the primaries as a function of aperture angle and reflection azimuth
to attenuate them. This is the focus of my current research.
Next: Acknowledgments
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Stanford Exploration Project
5/6/2007