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

S. L. Shvartsev

Результат исследований: Материалы для журналаСтатья

4 Цитирования (Scopus)

Выдержка

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.

Язык оригиналаАнглийский
Страницы (с-по)465-475
Число страниц11
ЖурналRussian Journal of Pacific Geology
Том2
Номер выпуска6
DOI
СостояниеОпубликовано - 2008

Отпечаток

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

ASJC Scopus subject areas

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

Цитировать

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

В: Russian Journal of Pacific Geology, Том 2, № 6, 2008, стр. 465-475.

Результат исследований: Материалы для журналаСтатья

@article{d1c655747a2a48c899a0242a20c09b86,
title = "Interaction in the water-rock system as a new basis for the development of hydrogeology",
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.",
keywords = "Equilibrium, Evolution, Geochemical type of water, Groundwater, Hydrogenous mineral complex, Hydrogeology, Interaction, Rock",
author = "Shvartsev, {S. L.}",
year = "2008",
doi = "10.1134/S1819714008060018",
language = "English",
volume = "2",
pages = "465--475",
journal = "Russian Journal of Pacific Geology",
issn = "1819-7140",
publisher = "Maik Nauka-Interperiodica Publishing",
number = "6",

}

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 -