PALEOZOIC DIKE SERIES IN THE KOLA ALKALINE PROVINCE: AGE AND CHARACTERISTICS OF MANTLE SOURCES

dc.contributor.authorArzamastsev A.A.
dc.contributor.authorArzamastseva L.V.
dc.contributor.authorTravin A.V.
dc.contributor.authorBelyatskii B.V.
dc.date.accessioned2022-01-16T05:05:34Z
dc.date.available2022-01-16T05:05:34Z
dc.date.issued2003
dc.description.abstractIn order to date the cessation of magmatic activity and characterize the final stage of Paleozoic magmatism in the northeast Baltic Shield, we carried out isotope-geochemical investigation of dikes that are abundant within the Kola region. Alkaline dikes are complex objects for dating. They lack zircon but contain alien mantle material and lower crustal xenoliths. Moreover, they are characternized by postmagmatic alterations and wall-rock assimilation. Therefore, we used a combination of Rb-Sr and Sm-Nd isochron determinations (internal mineral isochron) and 40Ar/39Ar methods These methods are described.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13444832
dc.identifier.citationDoklady Earth Sciences, 2003, 391, 6, 906-909
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/34365
dc.subjectPaleozoic
dc.subject.agePaleozoic
dc.subject.ageПалеозойru
dc.titlePALEOZOIC DIKE SERIES IN THE KOLA ALKALINE PROVINCE: AGE AND CHARACTERISTICS OF MANTLE SOURCES
dc.typeСтатья

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