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 language | English |
|---|---|
| Pages (from-to) | 465-475 |
| Number of pages | 11 |
| Journal | Russian Journal of Pacific Geology |
| Volume | 2 |
| Issue number | 6 |
| DOIs | |
| Publication status | Published - 2008 |
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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 journal › Article
}
TY - JOUR
T1 - Interaction in the water-rock system as a new basis for the development of hydrogeology
AU - Shvartsev, S. L.
PY - 2008
Y1 - 2008
N2 - 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.
AB - 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.
KW - Equilibrium
KW - Evolution
KW - Geochemical type of water
KW - Groundwater
KW - Hydrogenous mineral complex
KW - Hydrogeology
KW - Interaction
KW - Rock
UR - http://www.scopus.com/inward/record.url?scp=57349124914&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=57349124914&partnerID=8YFLogxK
U2 - 10.1134/S1819714008060018
DO - 10.1134/S1819714008060018
M3 - Article
AN - SCOPUS:57349124914
VL - 2
SP - 465
EP - 475
JO - Russian Journal of Pacific Geology
JF - Russian Journal of Pacific Geology
SN - 1819-7140
IS - 6
ER -