Seismic Imaging: a pratical approach

89 3. Seismic tomography 3.4 General conclusion This chapter, supported by several seismic field data examples, demonstrates the possibility of imaging the subsurface structures with seismic tomography. Seismic tomography is able: • to handle acquisitions of various scales and geometries; • to handle single or multi-component data; • to handle direct, reflected or diffracted P or S-body waves; • to produce high-resolution depth or time images; • to provide confidence criteria for the resulting tomogram. The main requirements for seismic tomography to build reliable images are: • high fold coverage; • large azimuthal coverage; • data that preserves travel times and amplitudes; • an initial model (P and/or S-wave velocity and density) that adequately represents the main subsurface features. • low or moderate computational effort. These tomograms may provide useful input data for further processing as pre or post-stack seismic migrations or for full waveform inversion techniques. References Aki K., Lee W.H.K., 1976, Determination of the three-dimensional velocity anomalies under a seismic array using first P arrival times from local earthquakes 1. A homogeneous initial model, J. Geophys. Res. 81, 4381-4399. Becquey M., Bernet-Rollande J.O., Laurent J., Noual G., 1992, Imaging reservoirs - a crosswell seismic experiment, First Break, 10 (9), 337. Beydoun W.B., Mendes M., Blanco J., Tarantola A., 1990, North Sea reservoir description: Benefits of an elastic migration/inversion applied to multicomponent vertical seismic profile data, Geophysics, 55 (2), 209-217. Beydoun W.B., Mendes M., 1989, Elastic ray-Born K2-migration/inversion, Geophys. J. 97, 151-160. Beydoun W.B., Delvaux J., Mendes M., Noual G., Tarantola A., 1989, Practical aspects of an elastic migration/inversion of crosshole data for reservoir characterization: A Paris basin example, Geophysics, 54 (12), 1587-1595. Brzostowski, M.A. and McMechan G. A., 1992, 3-D tomographic imaging of near-surface seismic velocity and attenuation, Geophysics, 57 (3), 396-403, https://doi.org/10.1190/1.1443254.

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