Magnetometric data traditionally were
widely used in applied and geological-
geophysical tasks. Primarily in such cases,
the area of interest is divided by magnetic
field characteristics. This procedure is to
be done either qualitatively or quantitatively
by using correlation analysis of data
[1].
Qualitative methods have no quantitative
criteria of field estimation and because
of that they are subjective. The correlation
analysis has digit characteristics, but in a
non-ordinary field, the following difficulties
could be met:
• in anomalous field spectrums, as usual,
several components are present and for
division the components of anomalous
field a priori knowledge of transformation
optimal parameters is necessary;
• some components of anomalous field
are piece-stationary.
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