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Abstract Machine contouring must not introduce information which is not present in the data. The one-dimensional spline fit has well defined smoothness properties. These are duplicated for two-dimensional interpolation in this paper, by solving the corresponding differential equation. Finite difference equations are deduced from a principle of minimum total curvature, and an iterative method of solution is outlined. Observations do not have to lie on a regular grid. Gravity and aeromagnetic surveys provide examples which compare favorably with the work of draftsmen.
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Ian Briggs (Fri,) studied this question.
synapsesocial.com/papers/6a1dd77666b24d664b6036be — DOI: https://doi.org/10.1190/1.1440410
Ian Briggs
University of Utah
Geophysics
Mineral Resources
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