Post-stack inversion of P-P Blackfoot data

Chanpen Silawongsawat


Various inversion algorithms will be run on migrated P-P Blackfoot data sets, in order to compare the pseudo-impedance sections of each method and, then, use the best method to compare inversions of P-P Blackfoot data, e.g. 2 Hz, 4 Hz, 10 Hz data collected with single geophones, and 10 Hz array data. Well logs from the area will be used as additional constraints for the inversions.

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