Some major matrix methods for computation of Green's functions of a layered
half-space model are compared. It is known that the original Thomson-Haske
ll propagator algorithm has the loss-of-precision problem when waves become
evanescent. The minor matrix extension solves to some extent the numerical
problem but at the expense of the computational efficiency. At present, th
e recursive technique (the reflectivity method) is used by most seismologis
ts. An alternative algorithm is presented that uses the same strategy as th
e original propagator algorithm but avoids the numerical problem by inserti
ng an additional numerical procedure into the matrix propagation loop. The
new technique is simple and efficient, and in particular, it is not only ap
plicable to the matrix method but also to any numerical integration method
for general use. High-frequency synthetic seismograms are computed for mode
ling significant site effects such as observed in the aftershocks of the La
tur earthquake, 1993, India.