The more mafic silicate rocks of the province originated from small degrees of partial melting in a source region in Earth's mantle made up of garnet-bearing peridotite. The lithosphere had thicknesses similar to present-day (200 km) conditions when magmas originated in the Devonian. Prior to Devonian magmatism the Kola and Karelia region had experienced a long history of low-frequency alkaline and carbonatite volcanism.[1]
The Permian rocks of the Kola Alkaline Province is commonly presumed to represent an igneous hotspot created by a mantle plume.[3] The relation of Kola Alkaline Province to other igneous or tectonic features is not clear. Some have suggested a link to the PermianDnieper-Donets Rift while others have considered it as part of a much larger a "North Atlantic Alkaline Province".[1]