SEP (Claerbout, 1999)
has traditionally taken an approach
which is described as either classical, traditional, or deterministic to iterative inversion.
The classical approach attempts to
find the model
that minimizes the data misfit. Given a recorded dataset
,
and a linear operator
, we attempt to minimize the
residual vector
which is defined as
(1)
In the simplest case
where we are using steepest
descent to solve the linear least squares inversion, we estimate
by mapping
the initial residual (in this simple case
) back into
the same space as the model to form a gradient vector
by
applying the adjoint of
. We then map the gradient vector back
into data-space by applying
to form
.
Finally, we find the scaling factor of
that will make
as small as possible. We then repeat this procedure
until
is suitably small. More complex inversion approaches
are normally built on this basic concept.