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Autocorrelation Functions in Geology

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Part of the book series: Computer Applications in the Earth Sciences ((CUOR))

Abstract

By using a method originally developed by P. Whittle, it is shown that a continuous random variable in three-dimensional space has an exponential autocorrelation function if it is subject to a property analogous to the Markov property in time-series analysis.

The problem of estimating autocorrelation functions from irregularly distributed map data is discussed. Approximate autocorrelation functions are shown for a set of 200 subsurface elevations on top of the Arbuckle Group (Cambrian-Ordovician) in Kansas. Trend-surface analysis, a method of kriging and a combination of the two procedures also are applied to the data. Areal interpolation can be done by a method that consists of three steps: (1) fitting a low-order polynomial trend surface; (2) estimation of the autocorrelation function for the residuals; (3) application of kriging to the residuals.

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© 1970 Plenum Press, New York

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Agterberg, F.P. (1970). Autocorrelation Functions in Geology. In: Merriam, D.F. (eds) Geostatistics. Computer Applications in the Earth Sciences. Springer, Boston, MA. https://doi.org/10.1007/978-1-4615-7103-2_10

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  • DOI: https://doi.org/10.1007/978-1-4615-7103-2_10

  • Publisher Name: Springer, Boston, MA

  • Print ISBN: 978-1-4615-7105-6

  • Online ISBN: 978-1-4615-7103-2

  • eBook Packages: Springer Book Archive

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