Geology Reference
In-Depth Information
Waterhead
complex
Field, prospect
Ater Palmer, %-экв.
Wa t e r
type ater
Sulin
2
+
+
+
r
r
Na
Cl
r
(
Cl Na
Mg
)
r
(Na Cl
SO
2
)
2
S
1
S
2
A
а
r
r
Lower Miocene
Borislav, Ivaniki,
Bitkov, Dzvinyach,
Pniv, Starunya,
Dobrogostov,
Orrov, Dolina etc.
81.3
-
85.7
12.9
-
17.8
-
0.9
-
1.4
0.82
-
0.88
-
1.93
-
3.22
ClCa
3
Upper
Cretaceous-
Upper
Oligocene
Tanyava, Spas,
Lukva, Bukhtovets,
Obolon, Bitkov,
Pniv, Dolina,
Kosmach,
Rosilyanovskoye,
Sloboda
Rungurskaya, etc.
77.1
-
86.7
0
-
21.4
0
-
11.4
1.5
-
1.9
0.79
-
1.15
-7.67
0.92
-
3.57
HCNa,
ClMg,
ClCa
Paleozoic-middle
Jurassic
77.5
-
78.0
21.5
-
21.8
-
0.5
-
0.7
0.79
-
0.80
-
3.19
-
3.78
ClCa
2
Sulin's characteristic of formation waters is based on the genetic principle. Under this principle, the ground water composition is formed in
continental, marine, deep environments as a result of water interaction with rocks of diferent genesis waters between themselves. In the process
they are enriched in speciic components based on which four water types are identiied (sulphate-sodium, hydrocarbonate-sodium, chloride-
magnesium and chloride-calcium). Each type is subdivided into three groups by anions (sulphate, hydrocarbonate and chloride) and into three
subgroups by cations (calcium, magnesium and sodium). Yandex.ru: http://www.drillings.ru/www/iles/klaspodzemvod.html.
3
Water types: ClCa (chlorine-calcium); HCNa (hydrocarbo
nate-sodium); ClMg (chloride-magnesium); SNa (sulphate-sodium).
