PECULIARITIES IN THE BEHAVIOR OF TRACE AND RARE EARTH ELEMENTS DURING GRANITIZATION AND MIGMATIZATION OF THE ELGAKAN COMPLEX (EAST SIBERIA, NYUKZHA RIVER)

dc.contributor.author	Glebovitsky V.A.
dc.contributor.author	Sedova I.S.
dc.contributor.author	Samorukova L.M.
dc.date.accessioned	2024-10-23T07:15:59Z
dc.date.available	2024-10-23T07:15:59Z
dc.date.issued	2006
dc.identifier	https://www.elibrary.ru/item.asp?id=13511087
dc.identifier.citation	Doklady Earth Sciences, 2006, 411, 8, 1309-1312
dc.identifier.issn	1028-334X
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/46152
dc.description.abstract	The behavior of major elements in the process of Neoarchean amphibolite-facies metamorphism was considered previously for occasionally pyroxene-bearing biotite–amphibole–plagioclase schists and amphibolites, which occur in the middle and lower reaches of the Nyukzha River and are identified as the Elgakan Unit. Ultrametamorphism took place in several stages. At the first stage, plagiogranite gneisses (Lc1) and rocks of an intermediate composition (sch*) were sequentially developed from the volume replacement of schists (sch).
dc.title	PECULIARITIES IN THE BEHAVIOR OF TRACE AND RARE EARTH ELEMENTS DURING GRANITIZATION AND MIGMATIZATION OF THE ELGAKAN COMPLEX (EAST SIBERIA, NYUKZHA RIVER)
dc.type	Статья
dc.identifier.doi	10.1134/S1028334X06080320

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