Foliation boudinage structures in the Mount Isa Cu system
Published in Australian Journal of Earth Sciences, 2023
B. J. Williams, T. G. Blenkinsop, R. Lilly, M. P. Thompson, P. Ila’ava
The world-class Mount Isa Cu and Pb–Zn deposit is located in the Mount Isa Inlier of northwest Queensland (Figure 1). Mount Isa Mine is the second-largest copper producer in Australia, producing approximately 6.5 Mt of ore per year up to 3.3 wt% Cu, with an estimated pre-mining total comprising 150 Mt at 7 wt% Zn and 6 wt% Pb, and 255 Mt at 3.3 wt% Cu (Glencore, 2022; Large et al., 2002, 2005; Potgieter, 2015). The Pb–Zn orebodies are generally close to the surface (Figure 2), where stratiform galena and sphalerite are hosted within dolomitic layers (Bell et al., 1988; Cave et al., 2020). The breccia dominated Cu ore bodies are located within a silica-dolomite alteration halo and occupy a deeper level in the Mount Isa system (Bell et al., 1988; Perkins, 1984; Swager, 1985). The Cu orebodies are typically discordant to bedding and interdigitate with the Pb–Zn orebodies (Bell et al., 1988; Cave et al., 2020; Perkins, 1984; Swager, 1985; Swager et al., 1987).