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Chromitite layers are common in large mafic layered intrusions. A widely accepted hypothesis holds that the chromitites formed as a consequence of injection and mixing of a chemically relatively primitive magma into a chamber occupied by more evolved magma. This forces supersaturation of the mixture in chromite, which upon crystallization accumulates on the magma chamber floor to form a nearly mon...

Origin of the UG2 chromitite layer, Bushveld Complex