Property Value
id 11089098
igsn 10.60494/3pez-g029
sample_id R011141D
eno 1083104
sampling_feature_name R011141D
sampling_feature_type field site
sample_type outcrop specimen
sampling_method outcrop sampling
material_class rock
stratigraphic_unit dolerite dyke, Smithton quarry
geological_province None
sample_remark Everard et al. 2023. MRT Report TR36: (This dolerite dyke) consists of scattered, partly altered olivine phenocrysts in a dominantly subophitic groundmass of titaniferous augite, plagioclase, titanomagnetite and partly altered mesostasis, with amygdales of carbonate and/or smectite.The olivine phenocrysts are generally +/- equant, <= 1.5 mm across, and partly (approx. 20%) to completely altered to a fibrous, pleochroic (pale to medium yellow-brown), strongly birefringent, length-slow alteration product, probably an amphibole and possibly anthophyllite. The bulk of the rock consists of a subophitic groundmass of pink-mauve titaniferous augite prisms (typically 500 micron-1mm ling [sic long] and 100-200 micon wide) and plagioclase laths (up to 600 x 100 um). Equant angular opaque grains, mostly 20-50 micron across are fairly abundant and are probably titanomagnetite/ulvospinel. There is some interstitial, strongly zoned but apparently untwinned feldspar (possibly alkali feldspar) and pale yellow-brown alteration (probably smectite). Numerous, round (mostly 0.5-1.5 mm diameter) to slightly flattened or irregular amygdales are filled with sparry carbonate and/or fine-grained pale brown smectite. In those amygdales in which both minerals are present, smectite forms the lining and carbonate the core.
earth_materials Y
structural_measurements None
inorganic_geochemistry None
organic_geochemistry None
geochronology None
isotope_groups None
hydrochemistry None
rock_properties None
mineralogy None
thin_sections None
repository_samples None
mineral_deposit_samples None
mineral_deposit_waste_samples None
linked_files None
other_geological_data None
project_name None
gda94_longitude 145.0991193
gda94_latitude -40.8454925
sample_originator Duncan, D.M.
date_acquired 3000-01-01 00:00:00
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