Abstract
The Middle Group (MG) chromitites of the Bushveld Complex host a substantial, largely untapped platinum-group element (PGE) resource, yet remain far less studied than the dominant UG2 chromitite and Merensky Reef. This review synthesises the published literature on the MG1–MG4A seams, covering stratigraphic setting, silicate and sulphide gangue mineralogy, platinum-group mineral and base-metal-sulphide relationships, and the comminution, flotation and comparative-metallurgy factors distinguishing MG processing from UG2 and Merensky practice, including the mineralogical drivers of circuit configuration and methods used to diagnose PGE losses to tailings. Four persistent gaps are identified: (i) absence of a reef-resolved PGM inventory across MG1–MG4A; (ii) limited data linking comminution and mineralogy to flotation reagent selectivity; (iii) an almost complete absence of published ore-blending studies; and (iv) a fragmented evidence base for MG-specific tailings reprocessing. Two recent, reef-resolved experimental studies from this research group are presented as a first step toward closing gaps (i) and (ii), and a three-part research agenda is set out a factorial blend-design programme, a standardised automated-mineralogy protocol, and an integrated gravity–magnetic–flotation circuit for MG tailings aimed at closing the remaining gaps and advancing Middle Group ore toward the geometallurgical maturity already achieved for UG2 and Merensky ore.