This work describes a simple stacking procedure based on summing the traces
of a common shot or common seismic section without the usual normal moveou
t (NMO) relative time shifts. We refer to this procedure as zero moveout (Z
MO) stacking. A simple horizontal summation with no shift in time results i
n a stacked trace that is the one-dimensional seismogram for horizontally l
ayered media. We explore the practical implementation of ZMO stacks for sou
rce estimation or wavelet extraction in deconvolution and/or identification
of source-reflector signatures necessary for performing inversion.