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Naturally, if we are given specific information
about the operator we can hope for better diagonal multiplers.
Most of the practical problems I am familiar with
are similar to the Radon transform
except that straight lines in the Radon transform become
various hyperbolas and hyperboloids.
The building blocks,
as you see from the Symes guess
and our follow-on guesses,
include using the data vector .We may also use vectors of ones and vectors of random numbers
in both data space and model space.
We can take spatial derivatives
in the geophysical model space ,and likewise space and time derivatives
in the data space .(The Radon transform special case
shows that we might even need half-order derivatives.)
We also have square roots of scalars and we have smoothing.
Next: UNITARITY
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Stanford Exploration Project
11/11/1997