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        "stratigraphic_unit":"unnamed pegmatite, Osborne mine",
        "geological_province":"Mount Isa Orogen",
        "sample_remark":"The Osborne copper and gold mine is 50 km south of Mount Dore and the deposit is hosted by quartzo-feldspathic gneisses interpreted to be high-grade equivalents of the Proterozoic Starcross Formation. Post- peak-metamorphic pegmatite sheet intrusions and minor lamprophyre dykes cut the host rocks. Adshead-Bell (1995) subdivided the sheet intrusions into three categories: i) porphyritic syenite, ii) alkali feldspar granite, and iii) pegmatites, and noted that they appear to be closely related in time because all intrusions post-date the peak of regional metamorphism and pervasive deformation but are overprinted by the economic mineralisation. This sample of pegmatite was collected to provide constraints on mineralisation at Osborne.",
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