ZIRCON GEOCHRONOLOGY OF THE SALDA METAMORPHIC COMPLEX, CENTRAL URALS

dc.contributor.author	Krasnobaev A.A.
dc.contributor.author	Davydov V.A.
dc.date.accessioned	2022-01-14T04:15:16Z
dc.date.available	2022-01-14T04:15:16Z
dc.date.issued	2003
dc.identifier	https://www.elibrary.ru/item.asp?id=13437651
dc.identifier.citation	Doklady Earth Sciences, 2003, 393, 9, 1247-1250
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/34312
dc.description.abstract	Investigations of zircon geochronology of the Salda metamorphic complex are continued in case of metamorphic rocks in eastern slope of Middle Urals. Results of the investigations make it possible to compare analytic and mineralogical-geochemical parameters of Salda metamorphic complex. Presence of nuclei and substrate fragments entrapped by the growing granulite crystals is base for 2195±68 million year geochronology. Conclusion about opportunity for non-total loss of Salda metamorphic complex memory on early stages of its existence has been made. Data on singleness of zircon formation and rock formation have been obtained. Using the zircon geochronology, similarity of geochronology boundaries of Middle Urals and Southern Urals has been noted.
dc.title	ZIRCON GEOCHRONOLOGY OF THE SALDA METAMORPHIC COMPLEX, CENTRAL URALS
dc.type	Статья

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