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Petrology of mafic lavas within the Onega plateau, central Karelia: evidence for 2.0 Ga plume-related continental crustal growth in the Baltic Shield

Onega PlateauMagmatic ProcessVolcanologyEngineeringIgneous PetrogenesisBaltic ShieldGeologyMafic LavasGeochemistryIgneous ProcessPetrologyIgneous PetrologyEarth ScienceTectonics