Inversion is an organized search for parameter values that maximize or
minimize an objective function, referred to here as a processor. This
note derives three new seismic processors that require neither prior
deconvolution nor knowledge of the source-receiver wavelet. The most p
owerful of these is the fourwise processor, as it is applicable to dat
a sets from multiple shots and receivers even when each shot has a dif
ferent unknown signature and each receiver has a different unknown imp
ulse response. Somewhat less powerful than the four-wise processor is
the pairwise processor, which is applicable cable to a data set consis
ting of two or more traces with the same unknown wavelet but possibly
different gains. When only one seismogram exists the partition process
or can be used. The partition processor is also applicable when there
is only one shot (receiver) and each receiver (shot) has a different s
ignature. In fourwise and pairwise inversions the unknown wavelets may
be arbitrarily long in time and need not be minimum phase. In partiti
on inversion the wavelet is assumed to be shorter in time than the dat
a trace itself but is not otherwise restricted. None of the methods re
quires assumptions about the Green's function.