U-PB ZIRCON DATING OF ROCKS OF THE PLATINIFEROUS FEDOROVA-PANA LAYERED MASSIF, KOLA PENINSULA

dc.contributor.authorNitkina E.A.
dc.date.accessioned2024-11-09T08:38:21Z
dc.date.available2024-11-09T08:38:21Z
dc.date.issued2006
dc.description.abstractThe Fedorova–Pana Massif (~400 km2 in area) located in the central Kola Peninsula belongs to the Northern belt of pyroxenite–gabbronorite PGE-bearing intrusions. The massif is confined to the junction of the Archean Keivy and Kola–Norwegian blocks in the north and Early Proterozoic Imandra–Varzuga structure in the south [3]. The Fedorova–Pana Massif incorporates the Fedorova, Lastjavr, Western Pana, and Eastern Pana blocks. The three latter blocks include “stratigraphic” (taxitic gabbronorite, norite, gabbronorite–gabbro) zones [4] with the ore-bearing Upper (ULH) and Lower (LLH) layered horizons.
dc.identifierhttps://www.elibrary.ru/item.asp?id=13529059
dc.identifier.citationDoklady Earth Sciences, 2006, 408, 4, 551-554
dc.identifier.doi10.1134/S1028334X06040106
dc.identifier.issn1028-334X
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/46444
dc.subjectFedorova–Pana massif
dc.subjectKola peninsula
dc.titleU-PB ZIRCON DATING OF ROCKS OF THE PLATINIFEROUS FEDOROVA-PANA LAYERED MASSIF, KOLA PENINSULA
dc.typeСтатья

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