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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