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PARAMETRIZATION OF GRT INVERSION FOR ACOUSTIC AND P–P SCATTERING1
- Source: Geophysical Prospecting, Volume 40, Issue 1, Jan 1992, p. 71 - 84
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- 27 Apr 2006
Abstract
The generalized Radon transform (GRT) inversion contains an explicit relationship between seismic amplitude variations, the reflection angle and the physical parameters which can be used to describe the earth efficiently for inversion purposes. Using this relationship, we have derived parametrizations for acoustic and P–P scattering so that the variations in seismic amplitude with reflection angle for each parameter are sufficiently independent. These parametrizations show that small offset and large offset amplitudes are related to different physical parameters. In the case of acoustic scattering, the small‐offset amplitudes are related to impedance variations while large‐offset amplitudes are related to velocity variations. A similar result has been established for P–P scattering.
The Born approximation (which is used to derive the GRT inversion) does not correctly predict the amplitude due to velocity variations at large offsets, and thus the inversion of velocity is not as satisfactory as the inversion of impedance.