Kirchhoff depth migration is a widely used algorithm for imaging seismic da
ta in both two and three dimensions. To perform the summation at the heart
of the algorithm, standard Kirchhoff migration requires a traveltime map fo
r each source and receiver. True-amplitude Kirchhoff migration in 2.5-D v(x
, z) media additionally requires maps of amplitudes, out-of-plane spreading
factors, and takeoff angles; these quantities are necessary for calculatin
g the true-amplitude weight term in the summation. The increased input/outp
ut (I/O) and computational expense of including the true-amplitude weight t
erm is often not justified by significant improvement in the final muted an
d stacked image. For this rea-son, some authors advocate neglecting the wei
ght term in the Kirchhoff summation entirely for most everyday imaging purp
oses.
We demonstrate that for nearly the same expense as ignoring the weight term
, a much better solution is possible. We first approximate the true-amplitu
de weight term by the weight term for constant-velocity media; this elimina
tes the need for additional source and receiver maps. With one small additi
onal approximation, the weight term can then be moved entirely outside the
innermost loop of the summation. The resulting Kirchhoff method produces im
ages that are almost as good as for exact true-amplitude Kirchhoff migratio
n and at almost the same cost as standard methods that do not attempt to pr
eserve amplitudes.