MULTIDIMENSIONAL SELF-AFFINE DISTRIBUTION WITH APPLICATION IN GEOCHEMISTRY

dc.contributor.authorWei Sh.
dc.contributor.authorPengda Zh.
dc.date.accessioned2021-04-16T05:17:18Z
dc.date.available2021-04-16T05:17:18Z
dc.date.issued2002
dc.description.abstractIn this paper, we present the conception of the multidimensional self-affine distribution and show that the multidimensional self-affine distribution possesses the fractal property of scale-invariance under truncation, which means that theoretical study of fractals has expanded from univariate cases to multivariate cases. Application of the multidimensional self-affine distribution is illustrated by means of geochemical Au and Ag elements data sets. The fractal dimension is a parameter which can quantitatively explain the variation of geochemical elements data on some orientation. This method is applied to Au data and Ag data, but also suited for other geochemical elements data or geological data. Theory of multivariate fractal can be applied for the study of change courses of fractal system, that is, fractal dynamics.
dc.identifierhttps://www.elibrary.ru/item.asp?id=950399
dc.identifier.citationMathematical Geology, 2002, 34, 2, 109-123
dc.identifier.issn0882-8121
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/27908
dc.subjectFRACTAL
dc.subjectFRACTAL DIMENSION
dc.subjectSCALE-INVARIANCE
dc.subjectPOWER LAW
dc.subjectVARIOGRAM
dc.titleMULTIDIMENSIONAL SELF-AFFINE DISTRIBUTION WITH APPLICATION IN GEOCHEMISTRY
dc.typeСтатья

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