The wavelet transform can be used to develop the process which allows
group and phase velocity measurement of dispersive waves. The method h
as been applied to acoustic data to measure formation velocities. The
behavior and the accuracy of the method have been checked on synthetic
full waveform acoustic data. The method was applied to dispersive wav
es of the Stoneley type and to flexural modes whose low frequency comp
onents are propagated at the formation shear velocity. A raw measureme
nt of the phase velocity of a flexural mode gives an estimate of the s
hear velocity with an error of about 5%. The use of a wavelet transfor
m yields an accurate study of dispersion and gives a shear velocity me
asurement with an error of less than 1%. However, all the examples pre
sented here are based on the use of synthetic data, which are not corr
upted by noise and were obtained with a numerical model. This algorith
m is complete, to the extent in which it enables simulation of all the
seismic arrivals for the considered geometry (cylindrical borehole wi
th a circular section, in an homogeneous medium). Nevertheless, such a
model remains a simplified version of what will occur in reality, whe
n the irregularities of the borehole, the cementing defects and the ba
ckground noise may call into question the excellent precision of the r
esults obtained. The process which is described in this paper must be
seen as one possible method for the analysis of field data, but it sti
ll has to be applied to many recordings of field data before its effec
tiveness can really be proved.