Abstract
The study of the saturation states of various underground waters (from ultra-fresh to strong brines) with different minerals show, that the water-rock system is in the equilibrium-nonequilibrium state. This internally contradictory state allows spontaneous, continuous evolution over geologically long time with the formation of principally new mineral phases and new geochemical types of water.
| Original language | English |
|---|---|
| Title of host publication | Water-rock interaction. Proc. symposium, Vladivostok, 1995 |
| Pages | 751-754 |
| Number of pages | 4 |
| Publication status | Published - 1995 |
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Environmental Science(all)