Interaction in the water-rock system as a new basis for the development of hydrogeology

S. L. Shvartsev

Research output: Contribution to journalArticle

4 Citations (Scopus)

Abstract

This paper addresses the main mechanisms controlling the continuous and geologically long evolution of the water-rock system, which produced diverse hydrogenous mineral complexes. The concept of such complexes was introduced by the author. It was shown that the water-rock system is a steady-state and equilibrium-disequilibrium one. Its development occurs in a far from equilibrium region and results in the formation of fundamentally new mineral associations and geochemical types of water. Taking into account that water is the main factor controlling the evolutionary trend of this system, it is argued that this system must be among the most important targets of hydrogeology.

Original languageEnglish
Pages (from-to)465-475
Number of pages11
JournalRussian Journal of Pacific Geology
Volume2
Issue number6
DOIs
Publication statusPublished - 2008

Fingerprint

hydrogeology
Hydrogeology
Rocks
rocks
Water
rock
water
Minerals
minerals
interactions
new mineral
disequilibrium
trends
mineral

Keywords

  • Equilibrium
  • Evolution
  • Geochemical type of water
  • Groundwater
  • Hydrogenous mineral complex
  • Hydrogeology
  • Interaction
  • Rock

ASJC Scopus subject areas

  • Geochemistry and Petrology
  • Geology
  • Geophysics
  • Oceanography
  • Palaeontology
  • Stratigraphy

Cite this

Interaction in the water-rock system as a new basis for the development of hydrogeology. / Shvartsev, S. L.

In: Russian Journal of Pacific Geology, Vol. 2, No. 6, 2008, p. 465-475.

Research output: Contribution to journalArticle

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