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Product Sheet: Depth Domain Inversion Services
Date: 6/3/2015
Quantitative interpretation in the depth domain
Conventional methods of amplitude inversion assume that amplitudes in the seismic image are correctly located and can be inverted to elastic parameters from which a true representation of rock properties can be derived. However, complex geology, combined with limitations imposed by surface seismic acquisition geometries, can lead to inadequate illumination of subsurface targets, which is detrimental to the amplitudes and phase of the migrated image.
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