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In this paper a simple procedure is shown that permits the estimation of resolution for a given set of data having specified measurement errors. For estimation of the resolution obtainable with a given set of data, it is not sufficient to combine the partial derivatives of the observed quantities with respect to the parameters at depth; since the resolution is severely limited by the errors of measurement, these errors must also be considered. The determination of shear velocity for the crust and upper mantle from surface-wave observations is considered as an example. The relative effectiveness of various combinations of modes for the determination of shear velocity is discussed.
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Der et al. (1970) studied this question.
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