Abstract
Strong calcium-chloride brines occur widely in sedimentary basins containing halide associations. Although several studies have been conducted on the origin of the brines, the detailed mechanisms, scales, and nature of these interactions remain debatable. The work reported here demonstrates that a water-aluminosilicate system has internal mechanisms capable of converting elements to dissolved form with their subsequent possible accumulation.
| Original language | English |
|---|---|
| Pages (from-to) | 246-250 |
| Number of pages | 5 |
| Journal | Transactions (Doklady) of the Russian Academy of Sciences. Earth science sections. |
| Volume | 344 |
| Issue number | 7 |
| Publication status | Published - Aug 1996 |
Fingerprint
ASJC Scopus subject areas
- Geology
- Geotechnical Engineering and Engineering Geology
Cite this
Role of rocks in producing strong calcium-chloride brines. / Shvartsev, S. L.; Bukaty, M. V.
In: Transactions (Doklady) of the Russian Academy of Sciences. Earth science sections., Vol. 344, No. 7, 08.1996, p. 246-250.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Role of rocks in producing strong calcium-chloride brines
AU - Shvartsev, S. L.
AU - Bukaty, M. V.
PY - 1996/8
Y1 - 1996/8
N2 - Strong calcium-chloride brines occur widely in sedimentary basins containing halide associations. Although several studies have been conducted on the origin of the brines, the detailed mechanisms, scales, and nature of these interactions remain debatable. The work reported here demonstrates that a water-aluminosilicate system has internal mechanisms capable of converting elements to dissolved form with their subsequent possible accumulation.
AB - Strong calcium-chloride brines occur widely in sedimentary basins containing halide associations. Although several studies have been conducted on the origin of the brines, the detailed mechanisms, scales, and nature of these interactions remain debatable. The work reported here demonstrates that a water-aluminosilicate system has internal mechanisms capable of converting elements to dissolved form with their subsequent possible accumulation.
UR - http://www.scopus.com/inward/record.url?scp=0030204532&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0030204532&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0030204532
VL - 344
SP - 246
EP - 250
JO - Transactions Doklady - Russian Academy of Sciences: Earth Science Sections
JF - Transactions Doklady - Russian Academy of Sciences: Earth Science Sections
SN - 1083-3552
IS - 7
ER -