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We obtained the known problem (1.40) for the impedance of a 1D medium with the
conductivity
D . The function Z ( z )in
the model under consideration evidently represents the normal impedance Z N ( z ).
Setting Z ( z )= Z N ( z ) and taking into account (10.43), (10.44) and (10.45), we find
the far-zone asymptotics
N ( z )
,
0
z
D and
D
=
const
,
z
>
| y y S | >> d =−
| y y S | >> d
(10
H A
H o z ( y )
H o y ( y )
i
o ( y
y S )
o z ( y )
i
o ( y
y S )
Z N (0)
=−
2
H A
2
o y ( y )
46)
that coincides with the known expression for a remote infinitely long linear current
(Vanyan, 1965). The normal impedance Z N (0) is connected with the ratio of the
components
.
H A
H A
0 y of the anomalous magnetic field, which can be determined
from values of the tipper W zy known at all points of the y- axis from -
0 z and
to
.To
H A
find
0 y , we solve the integral equation (5.80)
H A
o y ( y o )
1
W zy ( y ) H A
o y ( y )
+
dy o =−
W zy ( y )
.
y
y o
−∞
Then we compute
H A
o z
H A
=
W zy (1
+
o y )
(10
.
47)
.
H A
0 z
and calculate the normal impedance Z N from the far-zone asymptotics. With known
H A
Knowing W zy , we synthesize the normalized anomalous magnetic field
0 y ,
H A
H A
0 z and Z N , we integrate the second Maxwell equation (the Faraday law) and
continue the longitudinal impedance Z
0 y ,
to the entire y -axis:
.
y
E x ( y )
H y ( y ) =
1
H A
Z ( y )
=
Z N
i
o
o z ( y ) dy
(10
.
48)
H A
o y
1
+
−∞
Thus, we find Z from W zy . A one-to-one correspondence exists between Z and
W zy . Therefore, we can apply the Gusarov theorem (1981), stating that inversion of
Z has a unique solution, and extend this result to inversion of W zy . The uniqueness
theorem for 2D MT inversion (the TE-mode) gives rise to that for 2D MV inversion.
Moreover these two theorems can be supplemented by the uniqueness theorem for
the horizontal magnetic field.
IV. Return to a 2D model shown in Fig. 10.3. Let the longitudinal impedance
Z ( y )
Z ( y
=
,
z
=
0)
=
E x ( y
,
z
=
0)
/
H y ( y
,
z
=
0) be known at all
−∞
points of the y -axis from
to
in the entire range of frequencies
from 0 to
.
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