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is evidently distorted and should be shifted downwards to match the
xy - curve.
After correction we have two closely related
xy - and
yx -curves typical of a one-
dimensional model.
Lastly we consider a correction technique involving global magnetovariational
sounding, GMVS (Larsen, 1977; Rokityansky, 1982; Berdichevsky et al., 1989a, b;
Vanyan, 1997; Berdichevsky and Dmitriev, 2002). The technique is used to cor-
rect apparent-resistivity curves distorted by the
- and S- effects. Here the refer-
ence is given by the standard aparent-resistivity curve
st reproduced from GMVS
and large magnetotelluric statistics collected in different geological provinces. The
st -curve defines an average planetary distribution of the Earth's conductivity that
can be adopted as a normal geoelectric model of our planet. Figure 11.28 shows
the standard
st -curve suggested by Fainberg in his pioneering works (1983a, b).
It is composed of GMVS data and magnetotelluric extension that can be formed
by slightly distorted MT-curves obtained in different geological provinces. We will
use the
st -curve edited by Vanyan with regard to further generalizations of GMVS
and MT data (Vanyan, 1997; Berdichevsky et al., 1989a, b). Coordinates of this
st -curve are set out in Table 11.1. Figure 11.29 presents two examples of how
corrections are performed. Let a long-period apparent-resistivity curve
xy be dis-
torted by the
-effect that persists throughout the entire MT recording range. Its
low-frequency descending branch lies much below the
st -curve. To remove the
xy -curve should be shifted upward so that its low-frequency descend-
ing branch fits the
-effect, the
st -curve. In the case of the S -effect, the correction procedure
becomes more intricate. We have to take into account that the high-frequency
ascending branch of the
xy -curve reflecting the upper layer conductance is slightly
distorted and does not need any correction. So only the low-frequency branch of
Fig. 11.28 Constructing the
standard apparent-resistivity
curve
st
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