“…An understanding of ore formation in the northern lobe of has been made more complex, however, due a variety of factors such relatively poor outcrop as well as contamination of Bushveld Complex magmas with country rocks (Buchanan et al, 1981;Buchanan and Rouse, 1984;Cawthorn et al, 1985;Armitage et al, 2002). The occurrence of abundant footwall rafts and xenoliths, together with the disturbance of magmatic stratigraphy in the northern lobe bear testimony to the uniqueness of northern lobe rocks in comparison to those of the western and eastern lobes of the Bushveld Complex (Maier et al, 2021). The discovery of the Flatreef in the southern sector of the northern lobe permitted correlations with other lobes of the Bushveld Complex (Kruger, 1994;Roelofse et al, 2015) through the study of a magmatic stratigraphy less affected by footwall interaction such as strontium isotope ratios (Beukes et al, 2020), for example, and also with the northern sectors of the northern lobe (Buchanan et al, 1981;Gain and Mostert, 1982;Buchanan and Rouse, 1984;Yudovskaya et al, 2011).…”