The Pindos ophiolite complex, located in the north-western part of continental Greece, hosts various podiform chromite deposits generally characterized by low platinum-group element (PGE) grades. However, a few locally enriched in PPGE + Au (up to 29.3 ppm) chromitites of refractory type are also present, mainly in the area of Korydallos (south-eastern Pindos). The present data reveal that this enrichment is strongly dependant on chromian spinel chemistry and base metal sulfide and/or base metal alloy (BMS and BMA, respectively) content in chromitites. Consequently, we used super-panning to recover PGM from the Al-rich chromitites of the Korydallos area. The concentrate of the composite chromitite sample contained 159 PGM grains, including, in decreasing order of abundance, the following major PGM phases: Pd-Cu alloys (commonly nonstoichiometric, although a few Pd-Cu alloys respond to the chemical formula PdCu 4 ), Pd-bearing tetraauricupride [(Au,Pd)Cu], nielsenite (PdCu 3 ), sperrylite (PtAs 2 ), skaergaardite (PdCu), Pd-bearing auricupride [(Au,Pd) Cu 3 ], Pt and Pd oxides, Pt-Fe-Ni alloys, hollingworthite (RhAsS) and Pt-Cu alloys. Isomertieite (Pd 11 Sb 2 As 2 ), zvyagintsevite (Pd 3 Pb), native Au, keithconnite (Pd 20 Te 7 ), naldrettite (Pd 2 Sb) and Rh-bearing bismuthotelluride (RhBiTe, probably the Rh analogue of michenerite) constitute minor phases. The bulk of PGE-mineralization is dominated by PGM grains that range in size from 5 to 10 µm. The vast majority of the recovered PPGM are associated with secondary BMS and BMA, thus confirming that a sulphurbearing melt played a very important role in scavenging the PGE + Au content of the silicate magma from which chromian