Abstract
The Kostomuksha greenstone belt is the main iron district of Karelia. Gold, diamonds, and molybdenum mineralization have been found in this belt over the last two decades. The gold occurrences and deposits pertaining to the gold-sulfide and gold-quartz types were formed at the orogenic stage. The Taloveis deposit and the Faktorny and Berendei ore occurrences are located in the South Kostomuksha area and related to a complex of porphyritic diorite and granite porphyry. The West Ruvinvaara, Niemijarvi, Eastern, and Kurgelampi gold-sulfide and gold-sulfide-quartz occurrences are controlled by metasomatized shear zones and recrystallized sulfide ore hosted in the Shurlovaara and Ruvinvaara formations in the contact aureole of granite of the framework of the greenstone belt near its margin. The gold-arsenopyrite mineralization of the South Kostomuksha open pit is related to shear and metasomatic zones at the contact between the Kostomuksha Formation and helleflinta. Significant concentrations of gold are related to the complex of diorite and granite porphyry and the shear and metasomatic zones formed at the collision stage after emplacement of potassium granite. The small Taloveis deposit is located in the southern portion of the Kostomuksha greenstone belt and related to an intrusion of diorite and granite porphyry dated at 2720 Ma. The gold-sulfide mineral type in beresitized granite is combined with the gold-quartz type in shear zones trending at an azimuth of 20 NNE and coinciding in orientation with shear zones in the Kostomuksha belt. The Au grade varies from 0.5 to 60 g/t.
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References
V. M. Chernov, Stratigraphy and Deposition Conditions of Volcanogenic (Leptite) Banded Iron Formations in Karelia (Moscow, 1964) [in Russian].
V. Ya. Gor’kovets, M. B. Raevskaya, E. F. Belousov, and K. A. Inina, Geology and Metallogeny of the Kostomuksha Iron Deposit (Petrozavodsk, 1981) [in Russian].
V. Ya. Gor’kovets, M. B. Raevskaya, O. I. Volodichev, and L. S. Golovanova, Geology and Metamorphism of Banded Iron Formations of Karelia (Nauka, Leningrad, 1991) [in Russian].
V. N. Kozhevnikov, Formation Conditions of Precambrian Structural Metamorphic Associations (Nauka, Leningrad, 1982) [in Russian].
V. N. Kozhevnikov, Archaean Greenstone Belts of the Karelian Craton as Accretionary Orogens (Petrozavodsk, 2000) [in Russian].
L. V. Kuleshevich, “Evolution Stages of Gold Mineralization in the Kostomuksha Greenstone Belt,” in Proceedings of Scientific Conference Dedicated to the Tenth Anniversary of the Russian Foundation for Basic Research (Petrozavodsk, 2002a), p. 64.
L. V. Kuleshevich, “Felsic Magmatism and Gold Mineralization of the Kostomuksha Greenstone Belt,” in Geology and Mineral Resource of Karelia (Petrozavodsk, 2002b), No. 5, pp. 59–72 [in Russian].
L. V. Kuleshevich, “Evolution of Endogenetic Regimes and Stages of Gold Ore Formation in the Kostomuksha Greenstone Belt, Karelia,” Dokl. Akad. Nauk 396(6), 808–812 (2004) [Dokl. Earth Sci. 397 (5), 672–676 (2004)].
L. V. Kuleshevich and O. V. Vasyukova, “Formation Conditions of the Precambrian Taloveis Gold Deposit in Karelia,” Dokl. Akad. Nauk 403(6), 848–851 (2005) [Dokl. Earth Sci. 403A (6), 848–851 (2005)].
L. V. Kuleshevich, V. N. Furman, and N. N. Korotaeva, “The Berendei Gold Occurrence in the South Kostomuksha Ore Field,” in Geology and Mineral Resources in Karelia (Petrozavodsk, 2000), No. 2, pp. 50–59 [in Russian].
L. V. Kuleshevich, O. V. Vasyukova, and V. N. Furman, “Mineralogy and Formation Conditions of Gold Occurrences in the Kostomuksha Greenstone on Gas-Fluid Inclusion Data,” Zap. Ross. Mineral. O-va 134(5), 19–32 (2005).
Yu. O. Larionova, A. V. Samsonov, and A. A. Nosova, “The Rb-Sr Geochronology and Isotopic Geochemistry of Ore-Bearing Rocks and Wall-Rock Metasomatism of the Mesothermal Taloveis Gold Deposits, Western Karelia,” Dokl. Akad. Nauk 396(2), 239–243 (2004) [Dokl. Earth Sci. 396 (4), 525–528 (2004)].
S. B. Lobach-Zhuchenko, N. A. Arestova, R. I. Mil’kevich, O. A. Levchenkov, and S. A. Sergeev, “Stratigraphy of the Kostomuksha Belt in Karelia (Upper Archean) as Inferred from Geochronological, Geochemical, and Isotopic Data,” Stratigr. Geol. Korrelyatsiya 8(4), 3–10 (2000) [Stratigr. Geol. Correlation 8 (4), 319–326 (2000)].
S. B. Lobach-Zhuchenko, V. P. Chekulaev, V. V. Ivanikov, et al., “Late Archaean High-Mg and Subalkaline Granitoids and Lamprophyres as Indicators of Gold Mineralization in Karelia (Baltic Shield), Russia,” in Ore-Bearing Granites of Russia and Adjacent Countries (IMGRE, Moscow, 2000), pp. 193–211 [in Russian].
L. P. Nikitina, K. I. Lokhov, L. K. Levsky, et al., “Proterozoic Lamproite Magmatism of the Eastern Part of the Baltic Shield,” Vestn. St. Petersburg. Gos. Univ., Ser. 7 2(14), 11–24 (1999).
V. Yu. Prokof’ev, L. V. Kuleshevich, A. V. Volkov, and A. A. Sidorov, “The First Data on Formation Conditions and Composition of the Ore-Forming Fluids in Gold Occurrences of the Kostomuksha Iron Deposit, Karelia,” Dokl. Akad. Nauk 402(2), 233–238 (2005) [Dokl. Earth Sci. 402 (4), 582–586 (2005)].
I. S. Puchtel, A. W. Hofman, K. P. Yochum, et al., “The Kostomuksha Greenstone Belt, NW Baltic Shield: Remand of a Late Archaean Oceanic Plateau,” Terra Nova, No. 9, 87–90 (1997).
I. S. Puchtel, A. V. Samsonov, A. A. Shchipansky, and V. N. Furman, “Accretionary Tectonics in the Karelian Granite-Greenstone Region. The Kostomuksha Greenstone Belt As an Example of Terrane Structure,” in Proceedings of the I International Conference on Correlation of Geological Complexes of Fennoscandian Shield” (St. Petersburg, 1996), pp. 65–67.
A. V. Samsonov, I. S. Puchtel, E. V. Bibikova, and D. Z. Zhuravlev, “Petrology and Geochronology of Felsic Volcanic and Plutonic Rocks of the Kostomuksha Greenstone Belt, Western Karelia,” in Precambrian of Europe: Abstracts (IPPGG RAS, St. Petersburg, 1995), p. 95.
A. V. Samsonov, I. S. Puchtel, A. A. Shchiransky, and E. V. Bibikova, 2.72 Ga Sanukitoids of the Kostomuksha Greenstone Belt: Petrology and Tectonic Application (Svekalarko WS, Lammi, Finland, 1999), p. 58.
O. I. Volodichev, T. I. Kuzenko, and S. S. Kozlov, “Structure and Metamorphism of the Kontok Metavolcanics of the Kostomuksha Structure,” in Geology and Mineral Resources of Karelia (Petrozavodsk, 2002), No. 5, pp. 15–26 [in Russian].
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Original Russian Text © L.V. Kuleshevich, V. N. Furman, 2009, published in Geologiya Rudnykh Mestorozhdenii, 2009, Vol. 51, No. 1, pp. 58–76.
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Kuleshevich, L.V., Furman, V.N. The taloveis gold deposit in the precambrian Kostomuksha greenstone belt, Karelia. Geol. Ore Deposits 51, 51–67 (2009). https://doi.org/10.1134/S1075701509010048
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DOI: https://doi.org/10.1134/S1075701509010048