Equilibrium-nonequilibrium state of the water-rock system

S. L. Shvartsev

    Research output: Chapter in Book/Report/Conference proceedingChapter

    10 Citations (Scopus)

    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 languageEnglish
    Title of host publicationWater-rock interaction. Proc. symposium, Vladivostok, 1995
    Pages751-754
    Number of pages4
    Publication statusPublished - 1995

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    ASJC Scopus subject areas

    • Earth and Planetary Sciences(all)
    • Environmental Science(all)

    Cite this

    Shvartsev, S. L. (1995). Equilibrium-nonequilibrium state of the water-rock system. In Water-rock interaction. Proc. symposium, Vladivostok, 1995 (pp. 751-754)