GARNET PERIDOTITE XENOLITHS FROM ALKALIC PICRITOID AND BASANITOID OF THE VITIM PLATEAU

dc.contributor.author	Ashchepkov I.V.
dc.contributor.author	Dobretsov N.L.
dc.contributor.author	Kalmanovich M.A.
dc.date.accessioned	2020-04-15T06:24:13Z
dc.date.available	2020-04-15T06:24:13Z
dc.date.issued	1988
dc.identifier	https://elibrary.ru/item.asp?id=30975563
dc.identifier.citation	TRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 302, 5, 156-159
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16722
dc.description.abstract	Finds of garnet peridotite xenoliths in Cenozoic volcanics are fairly rare. Until recently, only three such finds were known on the Vitim plateau, in Pliocene rocks of the Kandiduskha and the Yasha paleo-volcanoes. We give the results of our study of 53 more garnet xenoliths from the same localities and of over 70 xenoliths from a new site - picritic basalt tuff, cropping our in a quarry. We propose a mechanism of upper mantle transformation for the Vitim Plateau.
dc.subject	Cenozoic	en
dc.subject	Pliocene	en
dc.title	GARNET PERIDOTITE XENOLITHS FROM ALKALIC PICRITOID AND BASANITOID OF THE VITIM PLATEAU
dc.type	Статья
dc.subject.age	Cenozoic	en
dc.subject.age	Cenozoic::Neogene::Pliocene	en
dc.subject.age	Кайнозой	ru
dc.subject.age	Кайнозой::Неоген::Плиоцен	ru

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