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.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.identifier	https://www.elibrary.ru/item.asp?id=13516239
dc.identifier.citation	Doklady Earth Sciences, 2006, 410, 7, 1096-1100
dc.identifier.doi	10.1134/S1028334X0607021X
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46240
dc.title	POLYGENOUS ZIRCONS IN THE ADUI BATHOLITH (MIDDLE URALS)
dc.type	Статья

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