Geology Reference
In-Depth Information
a
b
c
d
e
f
Figure 8.9
South Caspian Depression. Oil and gas reserve density in local structures vs.
geobaric conditions, extent of faulting, geothermal parameters and ground water vertical
mobility:
a. K
ан
=
f
(
d
i
,
K
ин
);
b. K
ан
=
f
(Г);
c. K
ан
=
f
(
h
a
);
d. K
ан
=
f
(
Н
з.п
);
e. М
=
f
(
K
ан
);
f. Qi
i
=
f
(
K
ан
). See Figure 7.5 for legend.
hydrodynamical systems in the South Caspian Depression: Balakhany-
Sabunchi-Ramany, Surakhany, Kala, Bibieybat and others. There, the
inverted hydrochemical disruptions of the high-salinity chlorine-calcium
regional background are genetically conjoined with discharge foci of the
desalinated high-thermal depth-generated alkaline waters. In the Tersk-
Caspian Trough, the fields are Karabulak-Achaluki, Malgobek-Voznesensk,
Orlinoye, Eldarovo and Khayan-Kort. There, positive concentration anom-
alies in the water medium of the Upper Cretaceous reservoir spatially cor-
respond with the areas of intense drainage of the Lower Cretaceous and
