FIRST RESULTS OF DATING OF ANABAR SHIELD ANORTHOSITES BY THE SM-ND ISOCHRON METHOD

dc.contributor.author	Sukhanov M.K.
dc.contributor.author	Spiridonov V.G.
dc.contributor.author	Karpenko S.F.
dc.date.accessioned	2020-10-31T07:55:31Z
dc.date.available	2020-10-31T07:55:31Z
dc.date.issued	1990
dc.identifier	https://elibrary.ru/item.asp?id=31091395
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1990, , 1, 174-177
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/18290
dc.description.abstract	Anorthosite of the independent type is a typical component of Precambrian granulite-gnesis, and the determination of its origin is very intimately related to a fundamental problem of geology, namely ascertaining the mode of evolution of the ancient continental crust. The popular radiometric dating methods do not work with anorthosite. which is a virtually monomineralic rock. In such a situation, Sm-Nd radiometric dating provides the most reliable results. The authors studied the Sm-Nd system in a simple of anorthosite from the Kotuykan group of plutons, confined to the Kotuykan zone of shear and diaphthoresis. Study methods and results are discussed.
dc.subject	Precambrian	en
dc.title	FIRST RESULTS OF DATING OF ANABAR SHIELD ANORTHOSITES BY THE SM-ND ISOCHRON METHOD
dc.type	Статья
dc.subject.age	Precambrian	en
dc.subject.age	Докембрий	ru

Files in this item

Files	Size	Format	View
There are no files associated with this item.