Property Value
id 2704878
igsn 10273/AU2704878
sample_id 2017843902
eno 626211
sampling_feature_name 17GRDD001
sampling_feature_type borehole
sample_type core
sampling_method core diamond
material_class rock
stratigraphic_unit unnamed mafic amphibolite
geological_province None
sample_remark Sample 2704878 is a fine- to medium-grained mafic amphibolite taken from the downhole interval 123.9–124.8 m in drillhole 17GRDD001. The mafic amphibolite is interpreted to intrude metasandstone of the Lander Rock Formation. The mafic amphibolite was selected for geochronology to determine its crystallisation age as it is spatially associated with mineralisation at the prospect. This area comprises mafic amphibolites of the Du Faur Suite, and rocks interpreted to be from the Andrew Young Igneous Complex. The mafic amphibolite sampled may represent part of the Du Faur Suite based on the low-K tholeiitic geochemical signature of the sample, which is consistent with the Du Faur Suite (Scrimgeour 2013). In thin section, the mafic amphibolite contains 40 –50 vol% amphibole, 30–40 vol% plagioclase, and 10 –20 vol% biotite, with feldspar-rich leucocratic patches/veins. The amphibole is commonly stubby to acicular, with lengths of 100–3000 μm and widths of 20–500 μm. The feldspar is anhedral with grain size in the range 50–1000 μm. Flaky biotite appears to replace the amphibole, with grain lengths of 20–200 μm and widths of 5–50 μm. Minor to trace minerals include oxide minerals, carbonate minerals and zircon.
earth_materials Y
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 EFTF - Isotopic Atlas of Australia
gda94_longitude 129.8385221
gda94_latitude -23.0633693
sample_originator Champion, D.C.
date_acquired None
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