EalesH. V.2000. Implications of the chromium budget of the Western Limb of the Bushveld Complex, South African Journal of Geology, 103, 141–150. doi: 10.2113/103.2.141
2.
IrvineT. N.1975. Crystallization sequences in the Muskox intrusion and other layered intrusions—II. Origin of chromitite layers and similar deposits of other magmatic ores, Geochimica et Cosmochimica Acta, 39, 991–1020. doi: 10.1016/0016-7037(75)90043-5
3.
LesherC. M., ArndtN. and GrovesD. I. 1984. Genesis of komatiite-associated nickel sulphide deposits at Kambalda, Western Australia: A distal volcanic model, in Sulphide deposits in mafic and ultramafic rocks, (eds. BuchananD. L. and JonesM. J.), 70–80; London, Institution of Mining and Metallurgy.
4.
LipinB. R.1993. Pressure increases, the formation of chromite seams, and the development of the Ultramafic Series in the Stillwater Complex, Montana, Journal of Petrology, 34, 955–976. doi: 10.1093/petrology/34.5.955
5.
MaierW. D., BarnesS.-J. and GrovesD. I.2013. The Bushveld Complex, South Africa: formation of platinum–palladium, chrome- and vanadium-rich layers via hydrodynamic sorting of a mobilized cumulate slurry in a large, relatively slowly cooling, subsiding magma chamber, Mineralium Deposita, 48, 1–56. doi: 10.1007/s00126-012-0436-1
6.
MondalS. K. and MathezE. A.2007. Origin of the UG2 chromitite layer, Bushveld Complex, Journal of Petrology, 48, 495–510. doi: 10.1093/petrology/egl069