Abstract
The abundance of various chemical elements (including trace, rare-earth, and radioactive) in the carbon dioxide mineral waters of the Choigan complex has been investigated. Three groups of waters are recognized according to the geochemical conditions and chemical composition: groundwaters of regional-jointing zone with oxidizing conditions; CO2-enriched groundwaters of regional-jointing zone with oxidizing conditions; and groundwaters of fault zones with reducing conditions. It is shown that water-rock interaction intensified by high temperature and carbon dioxide action is the main process determining the chemical composition of groundwaters.
| Original language | English |
|---|---|
| Pages (from-to) | 1295-1305 |
| Number of pages | 11 |
| Journal | Russian Geology and Geophysics |
| Volume | 55 |
| Issue number | 11 |
| DOIs | |
| Publication status | Published - 1 Jan 2014 |
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Keywords
- Carbon dioxide waters
- Chemical composition
- Choigan
- Tuva
- Water-rock interaction
ASJC Scopus subject areas
- Geology
- Geophysics
Cite this
Geochemistry of carbon dioxide mineral waters of the Choigan natural complex (northeastern Tuva). / Kopylova, Yu G.; Guseva, Natalia Vladimirovna; Arakchaa, K. D.; Khvashchevskaya, Albina Anatolievna.
In: Russian Geology and Geophysics, Vol. 55, No. 11, 01.01.2014, p. 1295-1305.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Geochemistry of carbon dioxide mineral waters of the Choigan natural complex (northeastern Tuva)
AU - Kopylova, Yu G.
AU - Guseva, Natalia Vladimirovna
AU - Arakchaa, K. D.
AU - Khvashchevskaya, Albina Anatolievna
PY - 2014/1/1
Y1 - 2014/1/1
N2 - The abundance of various chemical elements (including trace, rare-earth, and radioactive) in the carbon dioxide mineral waters of the Choigan complex has been investigated. Three groups of waters are recognized according to the geochemical conditions and chemical composition: groundwaters of regional-jointing zone with oxidizing conditions; CO2-enriched groundwaters of regional-jointing zone with oxidizing conditions; and groundwaters of fault zones with reducing conditions. It is shown that water-rock interaction intensified by high temperature and carbon dioxide action is the main process determining the chemical composition of groundwaters.
AB - The abundance of various chemical elements (including trace, rare-earth, and radioactive) in the carbon dioxide mineral waters of the Choigan complex has been investigated. Three groups of waters are recognized according to the geochemical conditions and chemical composition: groundwaters of regional-jointing zone with oxidizing conditions; CO2-enriched groundwaters of regional-jointing zone with oxidizing conditions; and groundwaters of fault zones with reducing conditions. It is shown that water-rock interaction intensified by high temperature and carbon dioxide action is the main process determining the chemical composition of groundwaters.
KW - Carbon dioxide waters
KW - Chemical composition
KW - Choigan
KW - Tuva
KW - Water-rock interaction
UR - http://www.scopus.com/inward/record.url?scp=84922638823&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84922638823&partnerID=8YFLogxK
U2 - 10.1016/j.rgg.2014.10.004
DO - 10.1016/j.rgg.2014.10.004
M3 - Article
AN - SCOPUS:84922638823
VL - 55
SP - 1295
EP - 1305
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
SN - 1068-7971
IS - 11
ER -