STRONTIUM ISOTOPIC COMPOSITION AND EVOLUTION OF A HYDROTHERMAL FLUID SOURCE: A CASE OF THE VEDUGA GOLD DEPOSIT, THE ENISEI RANGE

dc.contributor.authorChugaev A.V.
dc.contributor.authorBelov A.N.
dc.contributor.authorChernyshev I.V.
dc.date.accessioned2021-02-24T07:41:31Z
dc.date.available2021-02-24T07:41:31Z
dc.date.issued2001
dc.identifierhttps://elibrary.ru/item.asp?id=13384537
dc.identifier.citationDoklady Earth Sciences, 2001, 377 A, . С. 3, 362-364
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/25529
dc.titleSTRONTIUM ISOTOPIC COMPOSITION AND EVOLUTION OF A HYDROTHERMAL FLUID SOURCE: A CASE OF THE VEDUGA GOLD DEPOSIT, THE ENISEI RANGE
dc.typeСтатья

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