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Collaborating Authors
Results
The measured surface expression of the nagnetotelluric and controlled source data. It involves downward back-scattered field can then be used to reconstruct information diffusion of observed EM fields whose time flow has about the field inside the earth and, hence, the geoelectric been reversed. Unlike ordinary reversal of the process of structure (see Zhdanov and Frenkel, 1983a,b; Lee et diffusion, migration is a stable procedure that accurately restores al., 1987; and Zhdanov, 1988a,b).
anomalous structure, back-scattered field, back-scattered signal, Booker, diffusion equation, electromagnetic migration, Frenkel, geophysics, inversion, magnetotelluric data, migrated field, migration, primary field, Reservoir Characterization, seismic migration, structural information, underground imaging, Upstream Oil & Gas, Zhdanov
Country:
- Africa > South Africa > Western Cape Province > Indian Ocean (0.25)
- North America > United States (0.15)
- Europe (0.15)
Geophysics:
- Geophysics > Electromagnetic Surveying (0.54)
- Geophysics > Seismic Surveying (0.35)
SPE Disciplines: Reservoir Description and Dynamics > Reservoir Characterization > Seismic processing and interpretation (0.33)