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

dc.contributor.authorAshchepkov I.V.
dc.contributor.authorDobretsov N.L.
dc.contributor.authorKalmanovich M.A.
dc.date.accessioned2020-04-15T06:24:13Z
dc.date.available2020-04-15T06:24:13Z
dc.date.issued1988
dc.description.abstractFinds 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.identifierhttps://elibrary.ru/item.asp?id=30975563
dc.identifier.citationTRANSACTIONS (DOKLADY) OF THE USSR ACADEMY OF SCIENCES. EARTH SCIENCE SECTIONS, 1988, 302, 5, 156-159
dc.identifier.issn0891-5571
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/16722
dc.subjectCenozoicen
dc.subjectPlioceneen
dc.subject.ageCenozoicen
dc.subject.ageCenozoic::Neogene::Plioceneen
dc.titleGARNET PERIDOTITE XENOLITHS FROM ALKALIC PICRITOID AND BASANITOID OF THE VITIM PLATEAU
dc.typeСтатья

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