SULFIDE PGE-Cu-Ni AND LOW-SULFIDE Pt-Pd ORES OF THE MONCHEGORSK ORE DISTRICT (Arctic western sector): GEOLOGY, MINERALOGY, GEOCHEMISTRY, AND GENESIS
V.V. Chashchin1, V.N. Ivanchenko2
1Geological Institute of the Kola Science Center, Russian Academy of Sciences, ul. Fersmana 14, Apatity, 184209, Russia
2AO Rosgeologiya, ul. Odoevskogo 24, St. Petersburg, 199155, Russia
Keywords: Sulfide PGE-Cu-Ni and low-sulfide Pt-Pd ores, basal and reef types of deposits and manifestations, PGE geochemistry, platinum group minerals, Monchepluton, Monchetundra massif, Monchegorsk ore district
Abstract
During the recent exploration of the Monchegorsk ore district (MOD) in the Arctic western sector, the platinum potential of known Cu-Ni deposits (Nittis-Kumuzhya-Travyanaya (NKT), Nyud, Ore Horizon 330 (OH330), and Terrasa) has been assessed, and new sulfide PGE-Cu-Ni deposits (Western Nittis) and manifestations (Moroshkovoe Ozero, Poaz, and Arvarench), and low-sulfide Pt-Pd deposits (Loipishnyun, Southern Sopcha, and Vuruchuaivench) have been discovered. All of them are confined to Paleoproterozoic (ca. 2.5 Ga) layered intrusions (the Monchegorsk pluton (Monchepluton) and the Monchetundra massif) and are divided into two types according to their structural position: basal, located in the marginal parts of intrusions, and reef-type (stratiform). All types of ores show Pd specialization. Platinum group minerals (PGM) have a limited composition in sulfide PGE-Cu-Ni ores and are represented by predominant Pt and Pd compounds with Bi and Te and subordinate PGE arsenides and sulfides. Low-sulfide Pt-Pd ores are characterized by a significant variety of PGM, with a predominance of PGE sulfides, bismuthotellurides, and arsenides. Sulfide PGE-Cu-Ni deposits and manifestations (Western Nittis, NKT, Nyud, Moroshkovoe Ozero, Poaz, and Arvarench) formed through the accumulation of base metal sulfides and PGE in immiscible sulfides and their subsequent segregation in commercial contents. The reef-type OH330 deposit and Terrasa manifestation resulted from the injection of additional portions of sulfur-saturated magma. The basal-type low-sulfide Pt-Pd deposits (Loipishnyun and Southern Sopcha) formed from residual melts enriched in ore components and fluids separated and crystallized during long-term ore-forming processes. The reef-type Vuruchuaivench deposit is the result of deep fractionation of the parental magma with the formation of a sulfide liquid enriched in Cu and PGE. Significant reserves and large predicted resources of sulfide PGE-Cu-Ni and low-sulfide Pt-Pd ores are a reliable mineral resource base for the development of the mining industry in the Kola region of the Arctic western sector.
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