ANCIENT PLAGIOGNEISSES OF THE ONOT BLOCK OF THE SHARYZHALGAI METAMORPHIC MASSIF: ISOTOPIC GEOCHRONOLOGY

Bibikova E.V.; Kirnozova T.I.; Turkina O.M.; Fugzan M.M.

dc.contributor.author	Bibikova E.V.
dc.contributor.author	Kirnozova T.I.
dc.contributor.author	Turkina O.M.
dc.contributor.author	Fugzan M.M.
dc.date.accessioned	2024-11-02T11:07:53Z
dc.date.available	2024-11-02T11:07:53Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13523875
dc.identifier.citation	Geochemistry International, 2006, 44, 3, 310-315
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46367
dc.description.abstract	The oldest rocks found at Precambrian shields worldwide are so-called gray gneisses, which are high-grade metamorphic granitoids of predominantly tonalite composition. These rocks are often older than 3.6 Ga and mark the stage when the first sialic crust was produced. Such rocks with an age close to 3.6 Ga were found and dated in the former Soviet Union in the Ukrainian Shield and Omolon Massif in northeastern Siberia. The identification and reliable dating of each new area with these ancient rocks provides better insight into the timing of the origin of the Earth’s early crust and the scale and mechanisms of these processes.
dc.title	ANCIENT PLAGIOGNEISSES OF THE ONOT BLOCK OF THE SHARYZHALGAI METAMORPHIC MASSIF: ISOTOPIC GEOCHRONOLOGY
dc.type	Статья
dc.identifier.doi	10.1134/S0016702906030098