AR AND HE ISOTOPES IN THE DOVYREN MAFIC-ULTRAMAFIC INTRUSION

dc.contributor.authorKonnikov E.G.
dc.contributor.authorPrasolov E.M.
dc.contributor.authorTokarev I.V.
dc.contributor.authorKislov E.V.
dc.contributor.authorOrsoev D.A.
dc.date.accessioned2021-07-20T07:47:15Z
dc.date.available2021-07-20T07:47:15Z
dc.date.issued2002
dc.description.abstractThe paper presents results of Ar and He isotopic studies in rocks and sulfide ores of the Late Precambrian Dovyren dunite-troctolite layered intrusion (Northern Baikal region). The 3He/4He and 40Ar/36Ar ratios in the intrusion are similar to those in other mafic intrusions in the continental crust, and the gases in fluid inclusions bear a significant crustal component. The lowest 3He/4He and 40Ar/36Ar ratios in sulfide ores hosted by the intrusion, about those in crustal fluids, indicate involvement of the latter in magmatic mineralization.
dc.identifierhttps://elibrary.ru/item.asp?id=14995875
dc.identifier.citationGeologiya i geofizika, 2002, 43, 6, 543-552
dc.identifier.issn0016-7886
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/29773
dc.titleAR AND HE ISOTOPES IN THE DOVYREN MAFIC-ULTRAMAFIC INTRUSION
dc.typeСтатья

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