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 |
ASJC Scopus subject areas
- Geology
- Geotechnical Engineering and Engineering Geology