Information Technology Reference
In-Depth Information
Fig. 9.1
The
two-dimensional model with
conductive faults bordering
the central sedimentary
segment (a) and its equivalent
electric circuit (b)
where
S
1
(
y
)
h
2
. With regard to (9.1), this equation falls
into three independent equations with constant coefficients:
=
h
1
/
1
(
y
) and
h
=
h
1
+
g
1
f
2
g
1
f
2
d
2
Z
⊥
(
y
)
dx
2
Z
N
Z
⊥
(
y
)
−
=−
y
≥
v
+
q
g
2
f
2
g
2
f
2
d
2
Z
⊥
(
y
)
dx
2
(9
.
3)
Z
N
Z
⊥
(
y
)
−
=−
v
+
q
≥
y
≥
v
g
f
2
g
f
2
d
2
Z
⊥
(
y
)
dx
2
Z
N
−
Z
⊥
(
y
)
=−
≤
≤
v,
0
y
where
g
1
,
g
2
,
g
3
are galvanic parameters:
1
S
1
R
2
1
S
1
R
2
1
S
1
R
2
g
1
=
g
2
=
g
=
S
1
=
h
1
/
1
S
1
h
1
/
1
R
2
=
R
2
=
=
h
2
2
h
2
f
,
f
,
f
are induction parameters:
