The Mineral Composition of Paleoproterozoic Metamorphosed Massive Sulfide Ores in the Kola Region (A Case Study of the Bragino Ore Occurrence, Southern Pechenga)

Author:

Kompanchenko A. A.,Voloshin A. V.,Bazai A. V.

Publisher

Pleiades Publishing Ltd

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference35 articles.

1. Akhmedov, A.M., Voronyaeva, L.V., Pavlov, V.A., et al., The gold content of the South Pechenga structural zone (Kola Peninsula): types of manifestations and prospects for identifying industrial gold contents, Regional Geol. Metallogen., 2004, no. 20, pp. 143–165.

2. Allen, R.L., Lunstrom, I., Ripa, M., Simeonov, A., and Christofferson, H., Facies analysis of of a 1.9 Ga, contintental margin, back-arc, felsic caldera province with diverse Zn–Pb–Ag–(Cu–Au) sulfide and Fe oxide deposits, Bergslagen Region, Sweden, Econ. Geol., 1996, vol. 91, pp. 979–1008.

3. Balashov, Y.A., Paleoproterozoic geochronology of the Pechenga–Varzuga structure, Kola Peninsula, Petrology, 1996, vol. 4, no. 1, pp. 1–22.

4. Bezmen, N.I., Tikhomirova, V.I., and Kosogova, V.P., Pyrite-pyrrhotite geothermometer: distribution of nickel and cobalt, Geokhimiya, 1975, no. 5, pp. 700–714.

5. Craig, J.R. and Vokes, F.M., The metamorphism of pyrite and pyritic ores: an overview, Mineral. Mag., 1993, vol. 57, pp. 3–18.

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