POLYGENOUS ZIRCONS IN THE ADUI BATHOLITH (MIDDLE URALS)

dc.contributor.author	Krasnobaev A.A.
dc.contributor.author	Fershtater G.B.
dc.contributor.author	Bea F.
dc.contributor.author	Montero P.
dc.date.accessioned	2024-10-27T02:28:42Z
dc.date.available	2024-10-27T02:28:42Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13516239
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1096-1100
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46240
dc.description.abstract	The Adui Massif, the largest batholith in the north-western paleocontinental zone of the Urals, is highly similar to the northern Murzinka Massif. These batholiths probably make up a single massif. The Adui Batholith is composed of granites of different compositions and ages. Biotite and two-mica (orthoclase and microcline) granites and younger adamellites prevail among the granites. These rocks are intruded by numerous pegmatite and aplite veins.
dc.title	POLYGENOUS ZIRCONS IN THE ADUI BATHOLITH (MIDDLE URALS)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X0607021X

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