EVOLUTION OF THE HYDROGEN-ISOTOPE COMPOSITION IN THE MAGMATIC ORE-FORMING PROCESS IN ERDENETUIEN OBO DEPOSIT

dc.contributor.author	Berzina A.P.
dc.contributor.author	Kuroda Y.
dc.contributor.author	Sotnikov V.I.
dc.date.accessioned	2020-11-02T08:03:33Z
dc.date.available	2020-11-02T08:03:33Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31164302
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 1, 192-194
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18410
dc.description.abstract	n the largest copper-molybdenum deposit in Asia, the Erdentuin Obo in the Mongolian People's Republic, there are igneous rocks that contain isotopically unusually 'light' hydrogen as compared with other deposits of the same type. This paper reports on an analysis of the factors specifically controlling the isotope composition of hydrogen in the magma system that generated this large-volume mineral deposit. The isotope analyses (32 of rocks, and four of hornblende and biotite) were done in Shinshu University, Japan.
dc.title	EVOLUTION OF THE HYDROGEN-ISOTOPE COMPOSITION IN THE MAGMATIC ORE-FORMING PROCESS IN ERDENETUIEN OBO DEPOSIT
dc.type	Статья

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