GEOCHRONOLOGICAL ASPECT OF THE GEOCHEMISTRY OF STABLE ISOTOPES IN GEOTHERMAL WATERS

dc.contributor.author	Ustinov V.I.
dc.contributor.author	Grinenko V.A.
dc.contributor.author	Taran Yu.A.
dc.contributor.author	Barsukov L.A.
dc.date.accessioned	2020-10-11T11:08:08Z
dc.date.available	2020-10-11T11:08:08Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31155107
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 5, 223-225
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17923
dc.description.abstract	The theoretical possibility of using stable isotopes for geochronological purposes, based on the kinetics of isotope exchange reactions, was demonstrated in a study of the distributions of the isotopes of light elements in water and sediments of the Red Sea. In the present paper we discuss procedural approaches to the use of stable isotopes for dating purposes and describe techniques for determining certain parameters of the hydrothermal system, i.e., the residence time of water in the heated zone and the rate at which solutions migrate to the surface. Availability of such information on the properties of geothermal reservoirs will improve the effectiveness of prospecting for thermal waters, and this fact also emphasizes the importance of such investigations in isotope geochemistry.
dc.title	GEOCHRONOLOGICAL ASPECT OF THE GEOCHEMISTRY OF STABLE ISOTOPES IN GEOTHERMAL WATERS
dc.type	Статья

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