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Menke W. Geophysical Data Analysis: Discrete Inverse Theory
Academic Press, Revised Edition 1989, 289 Pages

Every researcher in the applied sciences who has analyzed data has practiced inverse theory. Inverse theory is simply the set of methods used to extract useful inferences about the world from physical measurements. The fitting of a straight line to data involves a simple application of inverse theory. Tomography, popularized by the physician’s CAT scanner, uses it on a more sophisticated level.

The treatment of inverse theory in this book is divided into four parts. Chapters 1 and 2 provide a general background, explaining what inverse problems are and what constitutes their solution as well as reviewing some of the basic concepts from probability theory that will be applied throughout the text. Chapters 3 - 7 discuss the solution of the canonical inverse problem: the linear problem with Gaussian statistics. This is the best understood of all inverse problems; and it is here that the fundamental notions of uncertainty, uniqueness, and resolution can be most clearly developed. Chapters 8 - 1 1 extend the discussion to problems that are non-Gaussian and nonlinear. Chapters 12 - 14 provide examples of the use of inverse theory and a discussion of the numerical algorithms that must be employed to solve inverse problems on a computer.
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