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                <identifier>oai:data.mendeley.com/2p3fk8x8nr.1</identifier>
                <datestamp>2018-03-22T05:28:05Z</datestamp>
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    <dc:creator>Spry, Paul</dc:creator>
    <dc:title>Data for: The origin of the sediment-hosted Kanmantoo Cu-Au deposit, South Australia: Mineralogical considerations</dc:title>
    <dc:publisher>Mendeley Data</dc:publisher>
    <dc:description>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.</dc:description>
    <dc:subject>Economic Geology</dc:subject>
    <dc:contributor>Pollock, Meaghan</dc:contributor>
    <dc:contributor>Both, Ross</dc:contributor>
    <dc:contributor>Koenig, Alan</dc:contributor>
    <dc:contributor>Ogierman, Joseph</dc:contributor>
    <dc:contributor>Tott, Katherine</dc:contributor>
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    <dc:identifier>doi:10.17632/2p3fk8x8nr.1</dc:identifier>
    <dc:identifier>oai:data.mendeley.com/2p3fk8x8nr.1</dc:identifier>
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