Abstract
Role of Fluids in Origin PGE Mineralization’s in the Pansky Tundra Layered Intrusion, Kola Peninsula, NW Russia
Highlights
The Pansky Tundra layered intrusion belongs to a group of the Paleo Proterozoic layered intrusions (2.45-2.50Ga) located in the north-eastern Fennoscandian Shield, Kola Peninsula (Russia)
Ore-bearing altered pyroxene anorthosites are composed by two successively-formed metasomatic association: 1) replacement of pyroxene by tremolite and magnetite; 2) epidote-zoisite-chlorite-albite-sericite-quartz association in the paragenesis with the sulphide-PGE mineralization
The REE patterns of ore-bearing anorthosites are characterized by positive Eu-anomaly and lower contents of HREE
Summary
The Pansky Tundra layered intrusion belongs to a group of the Paleo Proterozoic layered intrusions (2.45-2.50Ga) located in the north-eastern Fennoscandian Shield, Kola Peninsula (Russia). Role of Fluids in Origin PGE Mineralization’s in the Pansky Tundra Layered Intrusion, Kola Peninsula, NW Russia. Role of Fluids in Origin PGE Mineralization’s in the Pansky Tundra Layered Intrusion, Kola
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