One of the problems with most geophysics techniques is they provide only
a single answer and no measure of the uncertainty of the estimation.
In Appendix
, I show how we can modify the way
we set up the inverse problem to obtain equi-probable results. By comparing
and contrasting these realizations we can better understand model variability
and uncertainty.
In Appendix
and
, I extend the concepts
introduced in Chapters
and
to 3-D.
Appendix
shows how a 3-D steering filter can be
constructed by cascading two 2-D filter. Finally, in
Appendix
, I derive a 3-D tau tomography operator.