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

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dc.contributor.author Nitkina E.A.
dc.date.accessioned 2024-11-09T08:38:21Z
dc.date.available 2024-11-09T08:38:21Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=13529059
dc.identifier.citation Doklady Earth Sciences, 2006, 408, 4, 551-554
dc.identifier.issn 1028-334X
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/46444
dc.description.abstract The 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.subject Fedorova–Pana massif
dc.subject Kola peninsula
dc.title U-PB ZIRCON DATING OF ROCKS OF THE PLATINIFEROUS FEDOROVA-PANA LAYERED MASSIF, KOLA PENINSULA
dc.type Статья
dc.identifier.doi 10.1134/S1028334X06040106


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