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Fig. 11.55
brd in the presence of strong near-
surface noise: NP and CP are, respectively, the near-surface and crustal prisms. The horizontal
scale of distances is given in kilometers, and the vertical scale of resistivities is given in logarithmic
units of Ohm
Pseudo-topographies of the apparent resistivity
·
m
sufficiently large depth (Singer and Fainberg, 1997). The upper layer
{ 1 ( x
,
y )
,
h 1 }
is characterized by conductance S 1 ( x
y ). Applying the Price-
Sheinmann boundary conditions (7.15) valid within the S 1
,
y )
=
h 1 / 1 ( x
,
interval, we write
H x ( x
,
y
,
h 1 )
H x ( x
,
y
,
0)
=
S 1 ( x
,
y ) E y ( x
,
y
,
0)
H y ( x
,
y
,
h 1 )
H y ( x
,
y
,
0)
=−
S 1 ( x
,
y ) E x ( x
,
y
,
0)
(11
.
23)
E x ( x
,
y
,
h 1 )
=
E x ( x
,
y
,
0)
E y ( x
,
y
,
h 1 )
=
E y ( x
,
y
,
0)
,
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