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An example of the automatic contouring of geoelectrical data

Published online by Cambridge University Press:  01 May 2009

P. F. Worthington
Affiliation:
Department of Geology, University of Birmingham, Birmingham B15 2TT

Summary

Isopachytes of boulder clay in an area of Northwest Lancashire have been constructed from borehole-controlled geoelectrical data by separately using manual and automatic contouring techniques. At the sites of later drillings, the known boulder-clay thicknesses compare favourably with those indicated by both contour distributions, suggesting that the automatic techniques have a useful application in problems of this kind.

Type
Articles
Copyright
Copyright © Cambridge University Press 1973

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References

Carpenter, E. W. & Habberjam, G. M. 1956. A tri-potential method of resistivity prospecting. Geophysics 21, 455–69.CrossRefGoogle Scholar
Crain, I. K. 1970. Computer interpolation and contouring of two-dimensional data: a review. Geoexploration 8, 7186.Google Scholar
Habberjam, G. M. & Watkins, G. E. 1967. The reduction of lateral effects in resistivity probing. Geophys. Prospect. 15, 221–35.CrossRefGoogle Scholar
Price, D., Wright, W. B., Jones, R. C. B., Tonks, L. H. & Whitehead, T. H. 1963. Geology of the Country around Preston. Mem. geol. Surv. G.B., H.M.S.O. London.Google Scholar
Rhind, D. W. 1971. Automated Contouring—an Empirical Evaluation of Some Differing Techniques. Cartogr. Jnl 8, 145–58.CrossRefGoogle Scholar
Walters, R. F. 1969. Contouring by Machine: A User's Guide. Bull. Am. Ass. Petrol. Geol. 53, 2324–40.Google Scholar
Worthington, P. F. 1972. A geoelectrical investigation of the drift deposits in Northwest Lancashire. Geol. J. 8, 116.CrossRefGoogle Scholar