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The Gabbro-Wehrlite Association in the Eastern Part of the Baltic Shield

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Geology and Metallogeny of Copper Deposits

Part of the book series: Special Publication No. 4 of the Society for Geology Applied to Mineral Deposits ((MINERAL DEPOS.,volume 4))

Abstract

Proterozoic mafic and ultramafic intrusive rocks are widespread in the Archaean Kuhmo greenstone belt, including three minor Ni—Cu deposits. Similar intrusions have also been found in the Koli area cutting Jatulian metasediments and the underlying granitoid basement. They are incorporated in the same magmatic association “the gabbro-wehrlite association” as the Ni-bearing intrusions of Pechenga. The cumulate sequences in the layered bodies include olivine, olivine-clinopyroxene, clinopyroxene, clinopyroxene-magnetite, and plagioclase-clinopyroxene-magnetite cumulates. Ti-rich amphibole and mica occur abundantly as postcumulus phases in ultramafic rocks. The chemical compositions of the minerals and rocks differ from those of the Pechenga intrusions, reflecting differences in the parent magmas and their fractionation stages. The parent magmas in eastern Finland and Pechenga are similar to picrites of the Suisaarian and Pechenga types, respectively.

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© 1986 Springer-Verlag Berlin Heidelberg

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Hanski, E. (1986). The Gabbro-Wehrlite Association in the Eastern Part of the Baltic Shield. In: Friedrich, G.H., Genkin, A.D., Naldrett, A.J., Ridge, J.D., Sillitoe, R.H., Vokes, F.M. (eds) Geology and Metallogeny of Copper Deposits. Special Publication No. 4 of the Society for Geology Applied to Mineral Deposits, vol 4. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-70902-9_10

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  • DOI: https://doi.org/10.1007/978-3-642-70902-9_10

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