Property Value
id 2771376
igsn 10273/AU2771376
sample_id UR18TJM075
eno 628648
sampling_feature_name UR18TJM075
sampling_feature_type field site
sample_type outcrop specimen
sampling_method outcrop sampling
material_class rock
earth_materials Y
stratigraphic_unit Knuckey Formation
geological_province McArthur Basin
sample_remark The analysed sample was collected from the lower half of the Knuckey Formation type section, which is located about 10 km south-southeast of Mount Vizard in southern Urapunga. The Knuckey Formation is estimated to be about 150 m thick in the type section (Abbott et al 2001); the sample site is estimated to be 30–40 m stratigraphically above the base of the formation. The sample site is located in the bed of an unnamed ephemeral creek; sparse exposures are confined to the creek bed, and consist of low pavements and tabular to blocky rubble of thinly bedded, ripple-marked, fine-grained, light brown sandstone with a surficial dark grey colour. The sample is of a slightly weathered, fine-grained quartz-lithic sandstone, consisting of about 85% poorly sorted, angular to sub-rounded, to rarely well-rounded quartz grains, up to about 15% lithic grains (claystone rip-up clasts and chert grains), minor elongate muscovite, very rare labile grains (plagioclase, amphibole), and accessory zircon. Claystone clasts and muscovite grains tend to be aligned with bedding. Grains and clasts are set in a discontinuous, siliceous, authigenic quartz overgrowth cement that has been partially replaced by iron oxides as a result of weathering.
structural_measurements None
inorganic_geochemistry Y
organic_geochemistry None
geochronology Y
isotope_groups None
hydrochemistry None
rock_properties None
mineralogy None
thin_sections None
repository_samples Y
mineral_deposit_samples None
mineral_deposit_waste_samples None
linked_files None
other_geological_data None
project_name None
gda94_longitude 134.7830516
gda94_latitude -14.8853807
sample_originator Kositcin, N.
date_acquired None
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