Several operations enhance our ability to predict the subsurface below
the bottom total depth (TD) of the well when applied to zero-offset v
ertical seismic profiling (VSP) data. Other key issues regarding the u
se of vsp data in this fashion are resolution and look-ahead distance.
An impedance log is the most useful form for presenting VSP data to l
ook ahead of the drill bit. The VSP composite trace must first tie rel
iably to the surface seismic section and to the well log synthetic sei
smogram. The impedance log is obtained by inverting this VSP composite
trace. However, before performing forming the inversion, we need to (
1) correct the composite trace for attenuation effects below TD and (2
) input velocities to provide low-frequency information. An exponentia
l gain function applied to the VSP data below TD adequately compensate
s for the loss of amplitude caused by attenuation. A calibration of th
e seismically derived velocities with VSP velocities yields the necess
ary low-frequency information. These concepts are illustrated using a
field data set and its subset truncated above TD. The output of these
operations on the VSP data are compared to well log data. The question
of resolution with these data was determined with a model VSP data se
t based on the well log data. The investigations indicate that the res
olution attainable from look-ahead data is on the order of 50-75 ft (1
5-23 m). This is one-quarter seismic wavelength for the frequencies pr
esent in these data. In addition, the maximum look-ahead distance for
these data is shown to be easily 2000 ft (600 m) and, perhaps, 4000 ft
(1200 m). By way of illustration, the techniques described and invest
igated were applied to an offshore VSP data set to yield an impedance
log. After calibrating this curve with the well log data, the base of
the target sand was correctly identified below TD. This prediction suc
cessfully yielded the thickness of the sand. Individual zones within t
he sand unit were identified with less confidence.