Data for: The origin of the sediment-hosted Kanmantoo Cu-Au deposit, South Australia: Mineralogical considerations

Major element and trace element compositions of garnet, biotite, staurolite, chlorite, muscovite, and magnetite in metamorphosed altered rocks from the Kanmantoo deposit. Major elements compositions were obtained using a JEOL JXA-8900 Electron Probe Microanalyzer at the University of Minnesota. Trace element concentrations were measured at the U.S. Geological Survey in Denver, Colorado using laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS), comprising a Photon Machines Analyte LA system (excimer 193 nm) coupled to a PerkinElmer DRC-e ICP-MS.