The simulation of a zero-offset (ZO) stack section from multi-coverage refl
ection data is a standard imaging method in seismic processing. It signific
antly reduces the amount of data and increases the signal-to-noise ratio du
e to constructive interference of correlated events. Conventional imaging m
ethods, e.g., normal moveout (NMO)/dip moveout (DMO)/stack or pre-stack mig
ration, require a sufficiently accurate macro-velocity model to yield appro
priate results, whereas the recently introduced common-reflection-surface s
tack does not depend on a macro-velocity model. For two-dimensional seismic
acquisition, its stacking operator depends on three wavefield attributes a
nd approximates the kinematic multi-coverage reflection response of curved
interfaces in laterally inhomogeneous media. The common-reflection-surface
stack moveout formula defines a stacking surface for each particular sample
in the ZO section to be simulated. The stacking surfaces that fit best to
actual events in the multi-coverage data set are determined by means of coh
erency analysis. In this way, we obtain a coherency section and a section o
f each of the three wavefield attributes defining the stacking operator. Th
ese wavefield attributes characterize the curved interfaces and, thus, can
be used for a subsequent inversion. In this paper, we focus on an applicati
on to a real land data set acquired over a salt dome. We propose three sepa
rate one-parametric search and coherency analyses to determine initial comm
on-reflection-surface stack parameters. Optionally, a subsequent optimizati
on algorithm can be performed to refine these initial parameters. The simul
ated ZO section obtained by the common-reflection-surface stack is compared
to the result of a conventional NMO/DMO/stack processing sequence. We obse
rve an increased signal-to-noise ratio and an improved continuity along the
events for our proposed method - without loss of lateral resolution. (C) 1
999 Elsevier Science B.V. All rights reserved.