Rd. Miller et al., VERTICAL RESOLUTION OF A SEISMIC SURVEY IN STRATIGRAPHIC SEQUENCES LESS-THAN 100 M DEEP IN SOUTHEASTERN KANSAS, Geophysics, 60(2), 1995, pp. 423-430
A 400-m long, 12-fold high-resolution common depth point (CDP) reflect
ion seismic profile was acquired across shallow converging Pennsylvani
an strata in the Independence area of southeastern Kansas. One of the
principal objectives was to determine practical vertical resolution li
mits in an excellent shallow seismic-data area with borehole control.
The dominant frequency of the CDP stacked data is in excess of 150 Hz
based on peak-to-peak measurements. Interference phenomena observed on
stacked seismic data incorporated with models derived from log and dr
ill-hole information suggest a practical vertical resolution limit of
about 7 m, or one-third of the dominant wavelength. This practical res
olution is slightly less than the predicted (theoretical) resolution l
imit of 5 m based on the generally accepted one-quarter wavelength axi
om. These data suggest conventional rules of thumb describing resoluti
on potential are not accurate when reflectors on shallow, narrow bandw
idth data converge rapidly across horizontal distances less than the F
resnel Zone.