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        "sampling_method":"core diamond",
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        "geological_province":"Thomson Orogen",
        "sample_remark":"The sample was taken from drill-hole TDH6 at a depth interval of 855.54 to 856.50 metres. The drill-hole is situated very close to, and slightly south of, a prominent northeast-southwest-trending magnetic feature known as the Culgoa Shear Zone in the south-eastern Thomson Orogen (Doublier et al., 2018). The Culgoa Shear Zone defines the northern margin of a sedimentary depocentre of poorly-constrained age, known as the Paka Tank Trough. The sample analysed here is interpreted to come from the Paka Tank Trough. The sample is a fine-grained, grey-green, relatively massive rock with intermittent elongate quartz lenses aligned in a strong preferred orientation oblique to the core. At the time of core inspection the rock was interpreted as a possible volcanic, with the quartz lenses representing an original porphyritic texture. The rock was sampled for U-Pb geochronology to provide an age for volcanic activity and a stratigraphic age constraint on the surrounding sedimentary sequence. Subsequent petrographic observations suggest the rock is more likely a volcaniclastic sandstone rather than a lava.",
        "earth_materials":"Y",
        "structural_measurements":null,
        "inorganic_geochemistry":"Y",
        "organic_geochemistry":null,
        "geochronology":"Y",
        "isotope_groups":"Y",
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        "rock_properties":null,
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        "sample_originator":"Fraser, G.L.",
        "date_acquired":null
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