Intrabed multiples, either caused by shallow reverberations or the pre
sence of many thin layers, can have a detrimental effect on the signat
ure of deeper reflections. We discuss a method for removing these type
s of multiples. It can be viewed as a deterministic counterpart of wel
l-known predictive deconvolution methods and is aimed at estimating th
e inverse transmission operator of a subsurface region, directly from
its reflection response. The method is illustrated by applying it to b
oth synthetic and real data and appears to be able to reduce the effec
t of transmission intrabed multiples.