MacPhersons Reward gold deposit is in a post-kinematic tonalite intrusion which is a setting different from many other deposits of the Coolgardie goldfield that are hosted in early Archaean tholeiitic sills or meta-sedimentary rocks. Gold mineralisation at MacPhersons Reward consists of auriferous quartz veins that are best developed in the tonalite but extend to the adjacent komatiitic rocks and along the lithological contact zones. The gold-related alteration halo is dominated by biotite-chlorite and pyrrhotite. Unlike many other Coolgardie deposits, the As concentrations are low._x000D_
FORMAL CITATION:Goodz, M D, Phillips, G N and Money, L, 2011. Mine geology of the MacPhersons Reward Gold Mine, Coolgardie, Western Australia, in Proceedings Eighth International Mining Geology Conference 2011, pp 123-130 (The Australasian Institute of Mining and Metallurgy: Melbourne).