Special section on azimuthal dependence of P-wave seismic signatures—Introduction
This special issue is based on papers presented at the post‐convention SEG workshop on azimuthal dependence of P-wave signatures held in Dallas in 1997. The main motivation for analyzing the azimuthal variation of seismic traveltimes, amplitudes, attenuation, etc. is to obtain reliable information about azimuthal anisotropy in the subsurface. Another potential application of multiazimuth techniques is in finding and mapping desirable lateral heterogeneities that could “masquerade” as azimuthal anisotropy. The last topic has not yet been fully discussed (and is not addressed in the special issue), but several exploration and development scenarios contain oriented lateral heterogeneities (sand channels, etc.) that at the right scale length could be highly visible in properly processed wide‐azimuth 3-D data.