Abstract
Factorial kriging analysis is a new method which combines kriging analysis and principal component analysis into the framework of geostatistics. The variables are split into principal components corresponding to different frequency ranges.
It was tempting to apply this method to magnetic data, since the main objective of the study of these data is to determine the local structures that correspond to certain frequency ranges. In this paper, we present a few ways of applying this method to magnetism, and show the first results.
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References
Matheron, G., 1982: “Pour une analyse krigeante des données régionalisées”. Internal Report n° N-732, Centre de Géostatistique, Fontainebleau.
Matheron, G., 1981: “Splines and Kriging: their Formal Equivalence”. In “Down to Earth Statistics — Solutions looking for Geological Problems”, pp. 77–95, D.F. Merriam Editor, Syracuse University Geology Contributions.
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© 1984 D. Reidel Publishing Company, Dordrecht, Holland
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Galli, A., Gerdil-Neuillet, F., Dadou, C. (1984). Factorial Kriging Analysis: A Substitute to Spectral Analysis of Magnetic Data. In: Verly, G., David, M., Journel, A.G., Marechal, A. (eds) Geostatistics for Natural Resources Characterization. Springer, Dordrecht. https://doi.org/10.1007/978-94-009-3699-7_31
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DOI: https://doi.org/10.1007/978-94-009-3699-7_31
Publisher Name: Springer, Dordrecht
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