ARCHEAN AGE OF MIASKITE LAMPROITES FROM THE PANOZERO COMPLEX, KARELIA

dc.contributor.authorSergeev S.A.
dc.contributor.authorLarionov A.N.
dc.contributor.authorBerezhnaya N.G.
dc.contributor.authorLobach-Zhuchenko S.B.
dc.contributor.authorGuseva N.S.
dc.date.accessioned2026-06-01T10:45:20Z
dc.date.issued2007
dc.description.abstractUltrapotassic bodies classed with miaskite lamproite were found within the Archean Panozero magmatic complex on the southwestern coast of Lake Segozero, Central Karelia. The tectonic contacts of these bodies with host rocks make it impossible to determine their geological age and relations with the rocks of the Panozero Complex. The ages of previously studied ultrapotassic rocks are no older than Proterozoic. Compositionally close rocks were described only in the Udoks layered intrusion. Up to now, only nepheline syenites and carbonatites were known among Archean alkaline rocks. In this context, the isotope dating of the ultrapotassic rocks of the Panozero Complex is of special interest, because the data obtained may expand the age interval of potassic alkaline magmatism in the Early Precambrian.
dc.identifierhttps://elibrary.ru/item.asp?id=15292976
dc.identifier.citationDoklady Earth Sciences, 2007, 413, 3, 420-423
dc.identifier.doi10.1134/S1028334X07030221
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/53014
dc.subjectArchean
dc.subject.agePrecambrian::Archean
dc.subject.ageДокембрий::Архей
dc.titleARCHEAN AGE OF MIASKITE LAMPROITES FROM THE PANOZERO COMPLEX, KARELIA
dc.typeСтатья

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