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Noble metal mineralization of Motko and Kuolisma Proterozoic gabbrodolerite intrusions (Karelia)

Abstract

Results of studies of Proterozoic gabbrodolerite intrusions of Motko (2274 ± 3 Ma) and Kuolisma (1960 ± 2 Ma) in Central Karelia are reported. A brief description of their geological structure, degree of differentiation and rock composition is given. It is shown that noble metal mineralization is spatially combined with titanomagnetite horizon and associated with the formation of copper-sulfide mineralization. Platinum group metal minerals are mainly represented by palladium and platinum bismuthotellurids, arsenids and stibioarsenids with kotulskite and sperrylite being dominant. Chalkopyrite, bornite and chlorine-containing (up to 5.5 %) ferrogastingsite are indicator minerals of noble metal mineralization. Ore occurrences can be economically significant after additional appraisal.

About the Authors

V. I. Ivashchenko
Institute of Geology of Karelian Research Centre of the Russian Academy of Sciences (IG KarRC RAS)
Russian Federation

Candidate of Geological and Mineralogical Sciences, Leading Researcher



K. A. Konevin
ООО «Industriya»
Russian Federation

Geologist



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For citations:


Ivashchenko V.I., Konevin K.A. Noble metal mineralization of Motko and Kuolisma Proterozoic gabbrodolerite intrusions (Karelia). Regional Geology and Metallogeny. 2020;(84):97–105. (In Russ.)

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ISSN 0869-7892 (Print)