Property Value
id 2709120
igsn 10273/AU2709120
sample_id 2017848019
eno 11524
sampling_feature_name GSQ Westmoreland 2
sampling_feature_type borehole
sample_type half core
sampling_method core diamond
material_class rock
stratigraphic_unit Cliffdale Volcanics
geological_province Camooweal-Murphy Domain
sample_remark The unit sampled is a pink-red and green layered feldspar-rich fine to very fine ash-fall tuff within a thick felsic unit, sampled at depth 663.00-663.28 m in drillhole GSQ Westmoreland 2. Darby (1985; https://geoscience.data.qld.gov.au/report/cr013818) described this ash-fall tuff as having well developed planar bedding, defined by rectangular K-feldspar phenocrysts occurring in the same plane, parallel to their long dimensions, and other parallel variations in composition. The largest grains are about 2 mm, and consist of K-feldspar and plagioclase in a ratio of 1:2 respectively. They occur as euhedral crystals, often with their edges broken off. The groundmass consists of spherulitic intergrowths of quartz and plagioclase. Each spherulite has a coarse centre and much finer perimeter. Minor opaque minerals and aggregates of sericite also occur. This unit was targeted for SHRIMP zircon analysis to determine whether it is part of the c. 1850 Ma Cliffdale Volcanics (within the NE extension of the Murphy Inlier into Queensland), or part of a younger unit such as the c. 1725 Ma Peters Creek Volcanics of the lower McArthur Basin.
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 EFTF - Isotopic Atlas of Australia
gda94_longitude 138.3511699
gda94_latitude -17.4818683
sample_originator Champion, D.C.
date_acquired 2017-11-06 00:00:00
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