SECONDARY QUARTZITE IN THE POLAR URALS AS A REFERENCE POINT IN GEOLOGICAL HISTORY OF PASSIVE MARGIN OF THE EAST EUROPEAN CONTINENT

dc.contributor.author	Udoratina O.V.
dc.contributor.author	Silaev V.I.
dc.contributor.author	Delenitsyn A.A.
dc.date.accessioned	2022-01-12T07:50:48Z
dc.date.available	2022-01-12T07:50:48Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13425774
dc.identifier.citation	Doklady Earth Sciences, 2003, 391, 6, 823-826
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34233
dc.description.abstract	Discovery of apovolcanic aluminoquartzite with rare metal phosphate mineralization drastically changed the notions on mineragenic potential of Riphean metamorphic complexes in the Polar Urals. Until recently, it was believed that these metasomatites are directly related to the Riphean volcanism. However, we obtained new data on Middle-Late Ordovician age of the aluminoquartzite. These data have a great significance for the evolution of notions on the geological history and mineralogeny of the Polar Urals.
dc.title	SECONDARY QUARTZITE IN THE POLAR URALS AS A REFERENCE POINT IN GEOLOGICAL HISTORY OF PASSIVE MARGIN OF THE EAST EUROPEAN CONTINENT
dc.type	Статья

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