Interaction in the water-rock system as a new basis for the development of hydrogeology; Russian Journal of Pacific Geology; Vol. 2, iss. 6

Interaction in the water-rock system as a new basis for the development of hydrogeology; Russian Journal of Pacific Geology; Vol. 2, iss. 6

Bibliografiset tiedot
Parent link:Russian Journal of Pacific Geology
Vol. 2, iss. 6.— 2008.— [P. 465-475]
Päätekijä: Shvartsev S. L. Stepan Lvovich
Yhteenveto:Title screen
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.
Режим доступа: по договору с организацией-держателем ресурса
Kieli:englanti
Julkaistu: 2008
Aiheet:
электронный ресурс
труды учёных ТПУ
грунтовые подземные воды
гидрогеология
минеральные комплексы
геохимический тип воды
Linkit:http://dx.doi.org/10.1134/S1819714008060018
Aineistotyyppi: Elektroninen Kirjan osa
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=656194

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