Vibroseis data recorded at short source-receiver offsets can be swampe
d by direct waves from the source. The signal-to-noise ratio, where pr
imary reflections are the signal and correlation side lobes are the no
ise, decreases with time and late reflection events are overwhelmed. T
his leads to low seismic resolution on the vibroseis correlogram. A ne
w precorrelation filtering approach is proposed to suppress correlatio
n noise. It is the 'squeeze-filter-unsqueeze' (SFU) process, a combina
tion of 'squeeze' and 'unsqueeze' (S and U) transformations, together
with the application of either an optimum least-squares filter or a li
near recursive notch filter. SFU processing provides excellent direct
wave removal if the onset time of the direct wave is known precisely,
but when the correlation recognition method used to search for the fir
st arrival fails, the SFU filtering will also fail. If the tapers of t
he source sweeps are badly distorted, a harmonic distortion will be in
troduced into the SFU-filtered trace. SEU appears to be more suitable
for low-noise vibroseis data, and more effective when we know the swee
p tapers exactly. SFU requires uncorrelated data, and is thus cpu inte
nsive, but since it is automatic, it is not labour intensive. With non
-linear sweeps, there are two approaches to the S,U transformations in
SFU. The first requires the non-linear analytical sweep formula, and
the second is to search and pick the zero nodes on the recorded pilot
trace and then carry out the S,U transformations directly without requ
iring the algorithm or formula by which the sweep was generated. The l
atter method is also valid for vibroseis data with a linear sweep. SFU
may be applied to the removal of any undesired signal, as long as the
exact onset time of the unwanted signal in the precorrelation domain
is known or determinable.