Property Value
id 2169918
igsn 10273/AU2169918
sample_id HU13EEB139B
eno 575705
sampling_feature_name HU13EEB139B
sampling_feature_type field site
sample_type outcrop specimen
sampling_method outcrop sampling
material_class rock
stratigraphic_unit Mascotte Orthogneiss
geological_province Aileron Province
sample_remark A sample of equigranular to weakly porphyritic orthogneiss was collected from a site approximately 1.65 km west-southwest of Bonya Mine in northwestern JERVOIS RANGE. It is distinguished by well-developed centimetre-scale compositional banding with alternating layers of fine-grained granoblastic quartz and coarse-grained plagioclase and K-feldspar which are commonly partially, to wholly, saussuritised. Biotite comprises approximately 5% of the mineral mode and is largely altered to chlorite. Accessory minerals include abundant fine-grained magnetite and epidote. The gneiss is interpreted to have an igneous protolith of monzogranitic composition. This lithology is one of a variety of gneisses (and granites) currently assigned as part of the Mascotte Gneiss Complex on HUCKITTA (Freeman 1986). The Mascotte Gneiss Complex (Shaw et al 1984) has been interpreted to underlie the Bonya Schist with a transitional contact, and may form part of the same unit, but with a higher proportion of metaigneous rock. The Bonya Schist has a reported maximum depositional age of 1807 +/- 17 Ma (Claoue-Long and Hoatson 2005). The Complex is interpreted to have been intruded by the Jinka Granite (1714 +/- 3 Ma; Kositcin et al 2011).
earth_materials Y
structural_measurements None
inorganic_geochemistry Y
organic_geochemistry None
geochronology Y
isotope_groups Y
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 136.0507813
gda94_latitude -22.7284357
sample_originator Northern Territory Geological Survey (NTGS)
date_acquired None
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