Low mantle plume component in 370 Ma old Kola ultrabasic-alkaline-carbonatite complexes: Evidences from rare gas isotopes and related trace elements

dc.contributor.author	Tolstikhin, I.N.
dc.contributor.author	Kamensky, I.L.
dc.contributor.author	Nivin, V.A.
dc.contributor.author	Vetrin, V.R.
dc.date.accessioned	2021-10-21T06:31:15Z
dc.date.available	2021-10-21T06:31:15Z
dc.date.issued	1998
dc.identifier.citation	RUSSIAN JOURNAL OF EARTH SCIENCES, 1998, VOL. 1, NO. 2, p. 179–222	ru_RU
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/30843
dc.description.abstract	During Devonian pulse of alkaline magmatism (370 Ma ago) 18 ultrabasic-alkaline-carbonatite comlexes were formed on the Kola Peninsula.	ru_RU
dc.language.iso	en	ru_RU
dc.title	Low mantle plume component in 370 Ma old Kola ultrabasic-alkaline-carbonatite complexes: Evidences from rare gas isotopes and related trace elements	ru_RU
dc.type	Article	ru_RU
dc.subject.age	Paleozoic::Devonian
dc.subject.age	Палеозой::Девонская	ru

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