Reflector Maps and Earth Parameter
Estimation from Seismic Data: From
Ruler and Compass Construction to Gaussian Beam Propagators
Norman Bleistein,
Colorado School of Mines
Hagedoorn created a ruler and compass method for imaging reflectors in
the Earth for seismic exploration from pictures of the reflection
response in seismic data records. Although it was not apparent at the
time (1954), his method anticipated a hierarchy of asymptotic methods
for reflector imaging and estimation of geometrical optics or
ray-theoretic reflection coefficients via integral processes
reminiscent of a Green's function representation of solutions of the
wave equation from boundary data. Exploration geophysicists call the
basic method ``migration'' and the integral form, ``Kirchhoff
migration.'' Here, the data record in space-time has the appearance of
reflectors and thus the movement of that data from its temporal
location to its spatial location leads to the name ``migration.'' This
is the workhorse technique in the exploration geophysics community.
When the processing integral is properly weighted, the peak amplitude
of the image on each reflector is in know proportion to a reflection
coefficient at a determinable incidence angle. The method is then
referred to as ``true-amplitude migration'' or ``inversion,'' although
it is only a partial inversion that relies on low wave number
information about a background wave speed to propagate the data. This
talk describes the basic ideas and the use of ray-theoretic Green's
functions to propagate the observed data (and the source) into the
Earth. For about twenty years, Gaussian beam representations have been
used for Green's functions because of the smoother and more coherent
images that they produce, although the cost can be prohibitively and
non-competitively expensive.
Hill proposed a method for reducing the number of integrals and, hence,
the cost of this Kirchhoff processing with Gaussian beams. Moving that
less costly method from migration to true-amplitude migration has only
recently been achieved.
We describe this history as time allows.