Abstract
The sulphide copper-nickel deposits of the Pechenga ore field are confined to a profile running across the north-western part of the Kola peninsula (Atlas 1973; Gorbunov 1968; Yeliseev 1961). Most of the deposits are localized within the limits of the Pechenga ore field, being confined to the complex of the same name, and a lesser part was discovered in the Kola series. Ferruginous quartzites, muscovite-bearing pegmatites and hydrothermal lead-zinc veins are also known in the area under consideration.
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© 1987 Springer-Verlag Berlin Heidelberg
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Kozlovsky, Y.A. (1987). Ore Mineralization. In: Kozlovsky, Y.A. (eds) The Superdeep Well of the Kola Peninsula. Exploration of the Deep Continental Crust. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-71137-4_7
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DOI: https://doi.org/10.1007/978-3-642-71137-4_7
Publisher Name: Springer, Berlin, Heidelberg
Print ISBN: 978-3-642-71139-8
Online ISBN: 978-3-642-71137-4
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