IGNEOUS ACTIVITY AND METALLOGENY OF STRUCTURAL AND ASSOCIATIONAL ZONES WITH SIALIC BASEMENT IN THE URALS EUGEOSYNCLINE

dc.contributor.author	Smirnov V.N.
dc.contributor.author	Korovko A.V.
dc.contributor.author	Dvoyeglazov D.A.
dc.date.accessioned	2020-10-11T11:08:07Z
dc.date.available	2020-10-11T11:08:07Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31154951
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 4, 82-85
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17917
dc.description.abstract	Recent data indicate that even in the Urals, which constitute a reference femic type geosynclinal foldbelt, the geosynclinal structural and associational zones framing the ancient sialic blocks or microcontinents exhibit igneous rocks and endogenous metallogeny that differ from those in the principal, typically eugeosynclinal zones. In the present paper, the authors discuss the properties of such zones as exemplified by the Rezh structural and associational zone in the Central Urals.
dc.title	IGNEOUS ACTIVITY AND METALLOGENY OF STRUCTURAL AND ASSOCIATIONAL ZONES WITH SIALIC BASEMENT IN THE URALS EUGEOSYNCLINE
dc.type	Статья

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