REDUCED FLUID AS A FACTOR IN METAL MIGRATION

dc.contributor.author	Gottikh R.P.
dc.contributor.author	Pisotskiy B.I.
dc.contributor.author	Burmistenko Y.N.
dc.contributor.author	Spiridonov A.I.
dc.date.accessioned	2020-04-13T10:51:02Z
dc.date.available	2020-04-13T10:51:02Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30967458
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 300, 3, 162-165
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16682
dc.description.abstract	Judging by petrographic and f-radiographic data, a feature specific to such fluid is the presence in it of uranium. That explains why different categories of carbon compounds, generated as a result of its breakdown, also contain uranium. The aim of this work was to further study the trace-element composition of the fluid, the forms of their transport in it and their distribution patterns in the products of its breakdown. For this purpose, instrumental neutron-activation analysis was used. To determine the trace-element composition of the fluid, two quartz specimens were analyzed simultaneously. To study the aqueous phase, material from decrepitated vacuoles was first washed in doubly distilled water under nitrogen; then it was evaporated and analyzed. Study results ore discussed.
dc.title	REDUCED FLUID AS A FACTOR IN METAL MIGRATION
dc.type	Статья

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