Geology Reference
In-Depth Information
Table 9.1
(Cont.)
Region
Area
Correlation
ratio
Equations of the correlation
Q
i
=
f
(
K
ин
,
d
i
,
М
, Г,
K
ан
,
h
а
,
Н
з п
)
Indolo-Kuban trough
32
025
,
M
d
Γ
Q
=
0 008
,
M
⋅
Γ
0.992
i
i
025
,
d
127 48
,
0
,, 2 5
2
Q
=
50 25
,
i
−
+
13 33
,
K
⋅
Γ
0.905
(
)
i
025
,
aH
Γ
KK
⋅⋅
Γ
(
)
aH
И
H
Tersk-Caspian trough
,
025
025
,
Q MMK MM
011
,
3
043
,
i
=
⋅
Γ
⋅
−
()
0.994
(
)
И
025
,
025
,
2
KK
K
d
⋅
30 44
,
025
,
0.812
Q
858
,
И
H
4454
,
aH
И
H
006
,
Γ
dK
i
=
−
+
+
(
⋅
⋅
)
i
И
H
Γ
KK
025
,
⋅
i
aH
aH
Zagros trough
025
,
Γ
025
,
0.993
Q
i
=
14 59
,
H H K
⋅
Γ
3
⋅
H
−
11 57
,
H
(
)
∋
TT H
∋
И
∋
T
∋
T
K
2
aH
001
,
0
0002
025
,
Q
i
=
0 005
,
K
⋅
Γ
⋅
K
+
+
0 005
,
K
0,25
+
+
50 30
,
(
)
0.893
aH
И
H
И
H
025
,
025
,
K
⋅⋅
Γ
K
Γ⋅
K
И
(
)
(
)
И
H
aH
Total for the troughs
0.788
025
,
02
,
5
2
3
240 94
,
K
K
⋅
Γ
3
3
Q
i
=
aH
−
004
,
Γ
И
H
+
,
23 64
3
3
3
Γ
K
⋅
Γ
K
aH
И
H