We show both experimentally and theoretically how stress concentration
s affect the velocity field around a borehole, and how the velocity fi
eld influences dipole anisotropy measurements. At low frequencies the
dipole mode is sensitive to the far-field stresses primarily, so stand
ard sonic log interpretation correctly yields the direction of maximum
stress. At higher frequencies, the dipole mode is sensitive to near-f
ield stress concentrations such that the fast polarization direction i
s aligned with the direction of minimum tectonic stress. These effects
combine to produce a crossover in the dipole dispersion curves measur
ed in the fast and slow directions, With broad-band dipole data, the d
ispersion crossover can be used as an indicator of stress-induced anis
otropy dominating over weak intrinsic anisotropy.