Browsing by Author "Vetrin V.R."
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Browsing by Author "Vetrin V.R."
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Vetrin V.R.; Kamensky I.L.; Ikorsky S.V. (2003)
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Vetrin V.R.; Delenitsyn A.A.; Turkina O.M.; Ludden J. (2003)The basement of the Early Proterozoic Pechenga paleorift was penetrated by the Kola Superdeep Borehole at depths from 6842-12261 m. The main types of basement rocks are gneisses of dacite-plagiorhyodacite (tonalite-trondhjemite) ...
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Kamensky I.L.; Tolstikhin I.N.; Vetrin V.R. (1990)The 3He/4He in materials derived from the mantle is decreasing in the course of time and approaches the radiogenic value during {approx equal} 1 Ga. Some minerals, however, trapped volatiles, including He, and preserve ...
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Vetrin V.R.; Kamenskii I.L.; Ikorskii S.V.; Gannibal M.A. (2003)The He isotopic composition was studied in Archean enderbites, aluminous gneisses, and alkaline granites of the Kola Peninsula. It was shown that enderbites formed after intrusive protoliths during their granalite metamorphism ...
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Vetrin V.R.; Kamensky I.L.; Ikorsky S.V. (2001)
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Vetrin V.R.; Kamensky I.L.; Ikorsky S.V. (2002)The isotopic composition of He and Ar was analyzed in rocks and minerals from the Early Protero-zoic Litza-Araguba diorite-granite complex in the northwestern part of the Kola Peninsula. The initial 4He/3He ratio of the ...
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Beard A.D.; Downes H.; Hegner E.; Sablukov S.M.; Vetrin V.R.; Balogh K. (1998)Minor magmatic intrusions of kimberlite, melilitite and cpx-melilitite occur in the southern part of the Kola Peninsula, Russia, on the Terskii Coast and near the town of Kandalaksha. They yield K-Ar ages of 382 ± 14 Ma ...
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Vetrin V.R.; Kamenskiǐ I.L.; Delenitsin A.A.; Ikorskiǐ S.V. (2004)
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Vetrin V.R.; Turkina O.M.; Ludden J. (2002)The basement of the Early Proterozoic Pechenga paleorift was penetrated by the Kola Superdeep Borehole over a depth interval of 6842-12,261 m. The principal types of basement rocks are gneisses of trondhjemite-tonalite ...
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Vetrin V.R.; Delenitsin A.A. (2003)
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Tolstikhin I.N.; Kamensky I.L.; Nivin V.A.; Vetrin V.R.; Balaganskaya E.G.; Ikorsky S.V.; Gannibal M.A.; Marty B.; Weiss D.; Verhulst A.; Demaiffe D. (2002)During the Devonian magmatism (370 Ma ago) ∼20 ultrabasic-alkaline-carbonatite complexes (UACC) were formed in the Kola Peninsula (north-east of the Baltic Shield). In order to understand mantle and crust sources and ...
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Vetrin V.R. (2001)
Now showing items 1-12 of 12