Primary halos of one of the sulfide copper-nickel deposits in the north-west of the Kola Peninsula
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Abstract
The copper-nickel sulfide ore deposit under consideration is located in the northern part of the Tersko-Notozersky anticlinorium, composed predominantly of Archean rocks of the Kola series. Genetically and spatially, it is associated with a multilayer intrusion of ultrabasic rocks (olivinites, harzburgites) that are significantly metamorphosed. The intrusion is a series of bedded and lenticular bodies occurring in the nuclear part of the brachianticline, composed of rocks of the Kola gneiss series ...
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References
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