Page 32: of Offshore Engineer Magazine (Mar/Apr 2013)
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Geology & Geophysics
Figure 1 Figure 2.illustrates how the pressure (blue) and particle The image on the left is the result of seismic velocity (red) amplitude spectra are complementary when inversion applied to conventional seismic data containing measured at the same depth and location (‘collocated’). both source and receiver ghost effects. The color scale
Periodic notches in both spectra are related to the receiver represents ‘P impedance’: the product of compressional depth and the angle of emergence of the seismic wavefeld. velocity and density. In contrast, the right image represents
As the emergence angle increases (vertical propagation the ghost-free result provided from PGS GeoSource means zero emergence angle), the notches move to higher and dual-sensor GeoStreamer technologies. Note the frequencies. improvements in resolution on the right.
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OE | March 2013 oedigital.com 34 oe_PGS_rev2.indd 34 27/02/2013 13:22